# Vein Formation and Reopening in a Cooling Yet Intermittently Pressurized Hydrothermal System: The Single-Intrusion Tongchang Porphyry Cu Deposit

Xuan Liu, Antonin Richard, Jacques Pironon, Brian G Rusk

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Xuan Liu, Antonin Richard, Jacques Pironon, Brian G Rusk. Vein Formation and Reopening in a Cooling Yet Intermittently Pressurized Hydrothermal System: The Single-Intrusion Tongchang Porphyry Cu Deposit. Geosciences, 2023, 13, 10.3390/geosciences13040107. [https://doi.org/10.3390/geosciences13040107](https://doi.org/10.3390/geosciences13040107)

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# Vein Formation and Reopening in a Cooling Yet Intermittently Pressurized Hydrothermal System: The Single-Intrusion Tongchang Porphyry Cu Deposit

Xuan Liu, Antonin Richard, Jacques Pironon, Brian G Rusk

► To cite this version:

Xuan Liu, Antonin Richard, Jacques Pironon, Brian G Rusk. Vein Formation and Reopening in a Cooling Yet Intermittently Pressurized Hydrothermal System: The Single-Intrusion Tongchang Porphyry Cu Deposit. Geosciences, 2023, 13 (4), pp.107. 10.3390/geosciences13040107. [https://doi.org/10.3390/geosciences13040107](https://doi.org/10.3390/geosciences13040107)

HAL Id: hal-04621549

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Submitted on 24 Jun 2024

HAL is a multi-disciplinary open access
archive for the deposit and dissemination of sci-
entific research documents, whether they are pub-
lished or not. The documents may come from
teaching and research institutions in France or
abroad, or from public or private research centers.

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destinée au dépôt et à la diffusion de documents
scientifiques de niveau recherche, publiés ou non,
émanant des établissements d'enseignement et de
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Distributed under a Creative Commons Attribution 4.0 International License
Article

# Vein Formation and Reopening in a Cooling Yet Intermittently Pressurized Hydrothermal System: The Single-Intrusion Tongchang Porphyry Cu Deposit

Xuan Liu <fnref n="1" />*, Antonin Richard <fnref n="2" />, Jacques Pironon <fnref n="2" /> and Brian G. Rusk <fnref n="3" />

**Abstract:** Porphyry deposits are the dominant sources of copper and major sources of several base and precious metals. They are commonly formed via the repeated emplacement of hydrous magmas and associated fluid exsolution. As a result, mineralized hydrothermal veins may undergo multiple deposition and reopening processes that are not fully accounted for by existing fluid models. The Tongchang porphyry Cu deposit is a rare example of being related to a single intrusion. The simplicity in intrusive history provides an ideal starting point for studying fluid processes in more complex multi-intrusion porphyry systems. Detailed scanning electron microscope (SEM) cathodoluminescence imaging (CL) revealed rich micro textures in quartz and anhydrite that point to a fluid timeline encompassing early quartz deposition followed by fluid-aided dynamic recrystallization, which was succeeded by an intermediate stage of quartz dissolution and subsequent deposition, and ended with a late stage of continuous quartz deposition, brecciation, and fracturing. Vein reopening is more common than expected. Fifteen out of seventeen examined vein samples contained quartz and/or anhydrite that was older or younger than the vein age defined by vein sequences. Thermobarometry and solubility analysis suggests that the fluid events occurred in a general cooling path (from 650 °C to 250 °C), interspersed with two episodes of fluid pressurization. The first episode occurred at high-T (>500 °C), under lithostatic conditions alongside dynamic recrystallization, whereas the second one took place at a lower temperature (~400 °C), under lithostatic to hydrostatic transition conditions. The main episode of chalcopyrite veining took place subsequent to the second overpressure episode at temperatures of 380–300 °C. The results of this study reaffirm that thermal and hydraulic conditions are the main causative factors for vein reopening and growth in porphyry deposits.

**Keywords:** CL; quartz; anhydrite; solubility; hydrothermal process

## 1. Introduction

Porphyry deposits are the world's dominant sources of copper and molybdenum as well as important reservoirs of other base and precious metals [1]. They are one of the areas of focus of critical raw material studies [2]. The deposits are normally found along the convergent plate tectonic margins, formed via optimally-integrated magmatic and hydrothermal processes rooted in the subduction lithospheric mantle [3-7]. Despite several decades of studies, many details still await to be revealed, particularly regarding the mechanism of vein growth, reopening, and sulfide deposition [8-11].

The most widely-used porphyry fluid model classifies hydrothermal veins as early A-type quartz vein (700-550 °C), transitional B-type molybdenite quartz vein (500-400 °C), and late D-type pyrite veins (350-250 °C) based on vein morphology, mineralogy, and chronology. However, this model assumes that the veins are formed in a single event that

**Citation:** Liu, X.; Richard, A.; Pironon, J.; Rusk, B.G. Vein Formation and Reopening in a Cooling Yet Intermittently Pressurized Hydrothermal System: The Single-Intrusion Tongchang Porphyry Cu Deposit. *Geosciences* **2023**, *13*, 107. https://doi.org/10.3390/geosciences13040107

Academic Editor: Micol Bussolesi

Received: 20 February 2023

Revised: 18 March 2023

Accepted: 27 March 2023

Published: 1 April 2023

<figure><img src="image_2.png" /></figure>

**Copyright:** © 2023 by the authors. Licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license (https://creativecommons.org/licenses/by/4.0/).

<footnote n="1">¹ Geological Survey of Finland, P.O. Box 96, FI-02151 Espoo, Finland</footnote>

<footnote n="2">² GeoResources, CNRS, Université de Lorraine, F-54506 Vandoeuvre-lès-Nancy, France</footnote>

<footnote n="3">³ Department of Geology, Western Washington University, Bellingham, WA 98225, USA</footnote>

<footnote>* Correspondence: xuan.liu@gtk.fi; Tel.: +358-29-503-0074</footnote>
Article

# Vein Formation and Reopening in a Cooling Yet Intermittently Pressurized Hydrothermal System: The Single-Intrusion Tongchang Porphyry Cu Deposit

Xuan Liu 1*, Antonin Richard 2, Jacques Pironon 2 and Brian G. Rusk 3

**Abstract:** Porphyry deposits are the dominant sources of copper and major sources of several base and precious metals. They are commonly formed via the repeated emplacement of hydrous magmas and associated fluid exsolution. As a result, mineralized hydrothermal veins may undergo multiple deposition and reopening processes that are not fully accounted for by existing fluid models. The Tongchang porphyry Cu deposit is a rare example of being related to a single intrusion. The simplicity in intrusive history provides an ideal starting point for studying fluid processes in more complex multi-intrusion porphyry systems. Detailed scanning electron microscope (SEM) cathodoluminescence imaging (CL) revealed rich micro textures in quartz and anhydrite that point to a fluid timeline encompassing early quartz deposition followed by fluid-aided dynamic recrystallization, which was succeeded by an intermediate stage of quartz dissolution and subsequent deposition, and ended with a late stage of continuous quartz deposition, brecciation, and fracturing. Vein reopening is more common than expected. Fifteen out of seventeen examined vein samples contained quartz and/or anhydrite that was older or younger than the vein age defined by vein sequences. Thermobarometry and solubility analysis suggests that the fluid events occurred in a general cooling path (from 650 °C to 250 °C), interspersed with two episodes of fluid pressurization. The first episode occurred at high-T (>500 °C), under lithostatic conditions alongside dynamic recrystallization, whereas the second one took place at a lower temperature (~400 °C), under lithostatic to hydrostatic transition conditions. The main episode of chalcopyrite veining took place subsequent to the second overpressure episode at temperatures of 380–300 °C. The results of this study reaffirm that thermal and hydraulic conditions are the main causative factors for vein reopening and growth in porphyry deposits.

**Keywords:** CL; quartz; anhydrite; solubility; hydrothermal process

## 1. Introduction

Porphyry deposits are the world's dominant sources of copper and molybdenum as well as important reservoirs of other base and precious metals [1]. They are one of the areas of focus of critical raw material studies [2]. The deposits are normally found along the convergent plate tectonic margins, formed via optimally-integrated magmatic and hydrothermal processes rooted in the subduction lithospheric mantle [3-7]. Despite several decades of studies, many details still await to be revealed, particularly regarding the mechanism of vein growth, reopening, and sulfide deposition [8-11].

The most widely-used porphyry fluid model classifies hydrothermal veins as early A-type quartz vein (700-550 °C), transitional B-type molybdenite quartz vein (500-400 °C), and late D-type pyrite veins (350-250 °C) based on vein morphology, mineralogy, and chronology. However, this model assumes that the veins are formed in a single event that

**Citation:** Liu, X.; Richard, A.; Pironon, J.; Rusk, B.G. Vein Formation and Reopening in a Cooling Yet Intermittently Pressurized Hydrothermal System: The Single-Intrusion Tongchang Porphyry Cu Deposit. *Geosciences* **2023**, *13*, 107. https://doi.org/10.3390/geosciences13040107

Academic Editor: Micol Bussolesi

Received: 20 February 2023

Revised: 18 March 2023

Accepted: 27 March 2023

Published: 1 April 2023

<figure><img src="image_2.png" /></figure>

**Copyright:** © 2023 by the authors. Licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license (https://creativecommons.org/licenses/by/4.0/).

<footnote n="1">¹ Geological Survey of Finland, P.O. Box 96, FI-02151 Espoo, Finland</footnote>

<footnote n="2">² GeoRessources, CNRS, Université de Lorraine, F-54506 Vandoeuvre-lès-Nancy, France</footnote>

<footnote n="3">³ Department of Geology, Western Washington University, Bellingham, WA 98225, USA</footnote>

<footnote>* Correspondence: xuan.liu@gtk.fi; Tel.: +358-29-503-0074</footnote>
precipitates one generation of vein mineral. This assumption rarely holds for most porphyry deposits due to vein reopening, as revealed by several SEM-CL studies [12–18]. Erroneous interpretations on fluid source and conditions may result if they are based on bulk analyses of fluid inclusions, mineral chemistry, and isotopes of reopened veins.

Studies have shown that vein reopening in magmatic hydrothermal deposits may be linked to the number of igneous intrusions, which dictates the thermal and hydraulic properties of the system [8,19]. Ore deposits with a single intrusion may experience less reopening compared to multi-intrusion ones due to monotonic cooling, and thus less complicated hydraulic fracturing. The Tongchang Cu deposit is genetically associated with a single granodiorite intrusion [20]. This study presents a novel fluid model for the Tongchang Cu deposit by using integrated techniques of SEM-CL imaging [13,21,22], Ti-taniQ geothermobarometry [23–27], fluid inclusion microthermometry [13,28–30], and mineral solubility analysis [31,32].

## 2. Regional Geology

Most porphyry deposits form in terrains overriding subduction zones, where crustal magma chambers are fed by arc magmas [4]. Repetitive magma replenishment causes magma chambers to evolve chemically and mechanically, and drives the intrusion of multiple intrusive stocks [33]. In contrast, porphyry deposits with a single intrusion are rarely reported. Their scarcity is likely linked to the unique tectonic histories of the host terrain. The Tongchang porphyry deposit is a mono-intrusion system located in the inland of the South China Block (SCB), over 500 km from contemporaneous subduction belts [34] (Figure 1a). Interestingly, the deposit is situated within a much older subduction zone that sutured the SCB in the Neoproterozoic [35–37]. Despite the multiple reworking events in the Paleozoic and Mesozoic eras, geochemical and isotopic studies of the porphyry magmas have established connections with the Proterozoic subduction event [20,25,38,39]. For the sake of relevance and clarity, we describe Neoproterozoic and Mesozoic geology below.

<figure><img src="image_3.png" /><figcaption>**Figure 1.** (a) A satellite map showing the location of the South China Craton (SCC) and surrounding geologic terrains; (b) A geological map showing major lithologies and structures in the Phanerozoic era of SCC (adapted from [34]). AHF: Ailaoshan-Honghe Fault; CNF: Changle-Nanao Fault; JDF: Jingdezhen Fault; JNOB: Jiangnan Orogenic Belt; JSF: Jiangshan-Shaoxing Fault; LMF: Longmenshan Fault; HHF: Honghe Fault; NCC: North China Craton; NJF: Northeast Jiangxi Fault; QDOB: Qingling-Dabie Orogenic Belt; SMF: Song-Ma Fault; XMF: Xiangtan-Miluo Fault; XSF: Xianshuihe Fault; ZDF: Zhenghe-Dapu Fault. The yellow stars mark the location of the Dexing (including Tongchang) porphyry district.</figcaption></figure>

### 2.1. Neoproterozoic Geology
precipitates one generation of vein mineral. This assumption rarely holds for most porphyry deposits due to vein reopening, as revealed by several SEM-CL studies [12–18]. Erroneous interpretations on fluid source and conditions may result if they are based on bulk analyses of fluid inclusions, mineral chemistry, and isotopes of reopened veins.

Studies have shown that vein reopening in magmatic hydrothermal deposits may be linked to the number of igneous intrusions, which dictates the thermal and hydraulic properties of the system [8,19]. Ore deposits with a single intrusion may experience less reopening compared to multi-intrusion ones due to monotonic cooling, and thus less complicated hydraulic fracturing. The Tongchang Cu deposit is genetically associated with a single granodiorite intrusion [20]. This study presents a novel fluid model for the Tongchang Cu deposit by using integrated techniques of SEM-CL imaging [13,21,22], Ti-taniQ geothermobarometry [23–27], fluid inclusion microthermometry [13,28–30], and mineral solubility analysis [31,32].

## 2. Regional Geology

Most porphyry deposits form in terrains overriding subduction zones, where crustal magma chambers are fed by arc magmas [4]. Repetitive magma replenishment causes magma chambers to evolve chemically and mechanically, and drives the intrusion of multiple intrusive stocks [33]. In contrast, porphyry deposits with a single intrusion are rarely reported. Their scarcity is likely linked to the unique tectonic histories of the host terrain. The Tongchang porphyry deposit is a mono-intrusion system located in the inland of the South China Block (SCB), over 500 km from contemporaneous subduction belts [34] (Figure 1a). Interestingly, the deposit is situated within a much older subduction zone that sutured the SCB in the Neoproterozoic [35–37]. Despite the multiple reworking events in the Paleozoic and Mesozoic eras, geochemical and isotopic studies of the porphyry magmas have established connections with the Proterozoic subduction event [20,25,38,39]. For the sake of relevance and clarity, we describe Neoproterozoic and Mesozoic geology below.

<figure><img src="image_3.png" /></figure>

**Figure 1.** (a) A satellite map showing the location of the South China Craton (SCC) and surrounding geologic terrains; (b) A geological map showing major lithologies and structures in the Phanerozoic era of SCC (adapted from [34]). AHF: Ailaoshan-Honghe Fault; CNF: Changle-Nanao Fault; JDF: Jingdezhen Fault; JNOB: Jiangnan Orogenic Belt; JSF: Jiangshan-Shaoxing Fault; LMF: Longmenshan Fault; HHF: Honghe Fault; NCC: North China Craton; NJF: Northeast Jiangxi Fault; QDOB: Qingling-Dabie Orogenic Belt; SMF: Song-Ma Fault; XMF: Xiangtan-Miluo Fault; XSF: Xianshuihe Fault; ZDF: Zhenghe-Dapu Fault. The yellow stars mark the location of the Dexing (including Tongchang) porphyry district.

### 2.1. Neoproterozoic Geology
The eastern SCB comprises the Jiangnan Orogen and Cathaysia block [40] (Figure 1b), separated by the Jiangshan-Shaoxing Fault [37]. The orogen consists of three tectonic domains separated by the Northeast Jiangxi [41] (Figure 1b) and Xiangtan-Miluo faults [42]. The northeast domain is a volcanic arc terrain of arc-derived granite and volcanic rocks (970–880Ma [43]), with minor turbidite, ophiolitic mélange, and blueschists [44]. The central and southwest domains expose low-grade metamorphosed volcano-sediments and intruding S-type granites [41] (860–800 Ma). The volcano-sedimentary sequences are deposited in two periods, separated by an angular unconformity [45]. The underlying sequences are dominated by flysch-like successions of sandstone, siltstone, slate, and phylite deposited at 860–825Ma, including the Shuangqiaoshan Group in the northern Jiangxi and equivalents in other provinces [41,46]). The overlying sequence consists of slightly metamorphosed supracrustal rocks deposited in the Nanhua rift (e.g., the Banxi Group and equivalents [47]). The Cathaysia block comprises the Paleoproterozoic Badu Complex and Wuyishan granites as the basement, overlain by early Neoproterozoic volcanic successions (1000–900 Ma [48,49]). These rock associations have been interpreted as products of slab subduction [34,41,42,47,50,51].

## 2.2. Mesozoic Geology

The SCB is unconformably overlain by upper Neoproterozoic to lower Paleozoic, mid-Devonian to mid-Triassic, upper Triassic to lower Jurassic, and Cretaceous strata [34] (mainly clastic, volcanic and carbonate rocks, Figure 1b). The angular unconformities formed in three orogenic events in the Silurian, Triassic, and Jurassic eras [34]. Contemporaneous igneous activity was developed in large volumes. The Early Paleozoic (460–400 Ma) and Triassic (250–200 Ma) magmatic rocks are mainly S-type granites [52,53]. The Jurassic and Cretaceous igneous rocks are mainly A-type granite, syenite, and volcanic rocks, formed in two stages: i.e., 180–142 Ma and 142–67 Ma [53]. The early to middle Jurassic (190–170 Ma) is considered a period of magmatic quiescence with rock exposures only in the Dexing, Nanling and Qin-Hang regions [54]. Numerous tectonic models have been put forward for Mesozoic tectonics [34,53,55–62](Figure 1d), all suggesting that the Dexing region had undergone an intraplate extension during this time period [20,38,63].

## 3. Deposit Geology

The Tongchang deposit is one of three mineralizing centers in the Dexing Cu district (Figure 2). Along with Zhushahong and Fujiawu, the three deposits appear in the intersections of regional and local faults that delineate a NW-SE alignment. The three granodiorite porphyries are identical in mineralogy and rock chemistry [20,38], and emanated from a common batholith at depths confirmed by borehole drillings. Alteration patterns are clearly separated despite the fact that the intrusions are close to one another (Figure 2). The ore types are similar except for different Au and Mo contents.
The eastern SCB comprises the Jiangnan Orogen and Cathaysia block [40] (Figure 1b), separated by the Jiangshan-Shaoxing Fault [37]. The orogen consists of three tectonic domains separated by the Northeast Jiangxi [41] (Figure 1b) and Xiangtan-Miluo faults [42]. The northeast domain is a volcanic arc terrain of arc-derived granite and volcanic rocks (970–880Ma [43]), with minor turbidite, ophiolitic mélange, and blueschists [44]. The central and southwest domains expose low-grade metamorphosed volcano-sediments and intruding S-type granites [41] (860–800 Ma). The volcano-sedimentary sequences are deposited in two periods, separated by an angular unconformity [45]. The underlying sequences are dominated by flysch-like successions of sandstone, siltstone, slate, and phylite deposited at 860–825Ma, including the Shuangqiaoshan Group in the northern Jiangxi and equivalents in other provinces [41,46]). The overlying sequence consists of slightly metamorphosed supracrustal rocks deposited in the Nanhua rift (e.g., the Banxi Group and equivalents [47]). The Cathaysia block comprises the Paleoproterozoic Badu Complex and Wuyishan granites as the basement, overlain by early Neoproterozoic volcanic successions (1000–900 Ma [48,49]). These rock associations have been interpreted as products of slab subduction [34, 41, 42, 47, 50, 51].

## 2.2. Mesozoic Geology

The SCB is unconformably overlain by upper Neoproterozoic to lower Paleozoic, mid-Devonian to mid-Triassic, upper Triassic to lower Jurassic, and Cretaceous strata [34] (mainly clastic, volcanic and carbonate rocks, Figure 1b). The angular unconformities formed in three orogenic events in the Silurian, Triassic, and Jurassic eras [34]. Contemporaneous igneous activity was developed in large volumes. The Early Paleozoic (460–400 Ma) and Triassic (250–200 Ma) magmatic rocks are mainly S-type granites [52,53]. The Jurassic and Cretaceous igneous rocks are mainly A-type granite, syenite, and volcanic rocks, formed in two stages: i.e., 180–142 Ma and 142–67 Ma [53]. The early to middle Jurassic (190–170 Ma) is considered a period of magmatic quiescence with rock exposures only in the Dexing, Nanling and Qin-Hang regions [54]. Numerous tectonic models have been put forward for Mesozoic tectonics [34, 53, 55–62] (Figure 1d), all suggesting that the Dexing region had undergone an intraplate extension during this time period [20,38,63].

## 3. Deposit Geology

The Tongchang deposit is one of three mineralizing centers in the Dexing Cu district (Figure 2). Along with Zhushahong and Fujiawu, the three deposits appear in the intersections of regional and local faults that delineate a NW-SE alignment. The three granodiorite porphyries are identical in mineralogy and rock chemistry [20,38], and emanated from a common batholith at depths confirmed by borehole drillings. Alteration patterns are clearly separated despite the fact that the intrusions are close to one another (Figure 2). The ore types are similar except for different Au and Mo contents.
<figure><img src="image_4.png" /><figcaption>**Figure 2.** (a) A geological map of the Dexing porphyry Cu district; (b) Two cross sections (a–b, and c–d) of the Cu district (adapted from [19,38]). Dash lines denoted with L0-8 represents exploration lines; black pentagons represent the locations of drill hole, and the sampling localities are marked with small rectangles.</figcaption></figure>

### 3.1. Wall Rock and Intruding Porphyries

Wall rocks of the Dexing district are phyllite and tuffaceous slate of the Shuangqiaoshan Group (Figure 3a,b). Biotite and actinolite hornfels are developed in the wall rocks surrounding the granodiorites (Figure 3c). The granodiorites are obliquely emplaced, and account for over 95 vol.% of igneous intrusions in this district. They show porphyritic texture in the peripheral and upper part of the intrusions (Figure 3d), and the center and lower portions grade into an equigranular texture (Figure 3e). Phenocrysts and groundmass have similar mineral composition to andesine, K-feldspar, quartz, hornblende, and biotite. Both the granodiorite and wall rocks are hydrothermally altered and mineralized (Figure 3f). LA-ICP-MS zircon U-Pb dating suggested that the granodiorite formed at $171 \pm 3$ Ma [20,38,63], contemporaneous with Cu-Mo mineralization (molybdenite Re-Os age of ~170 Ma [64]). The porphyry magmas are interpreted as a partial melt of Neoproterozoic subduction-modified lithosphere [20,38]. There is minor (<5 vol.%) post-diorite porphyry and aplite (Figure. 3g–i). The diorite truncates mineralized veins (Figure 3h,i), and has been dated at ca. 154 Ma by the zircon U-Pb method [65].
<figure><img src="image_4.png" /><figcaption>**Figure 2.** (a) A geological map of the Dexing porphyry Cu district; (b) Two cross sections (a–b, and c–d) of the Cu district (adapted from [19,38]). Dash lines denoted with L0-8 represents exploration lines; black pentagons represent the locations of drill hole, and the sampling localities are marked with small rectangles.</figcaption></figure>

### 3.1. Wall Rock and Intruding Porphyries

Wall rocks of the Dexing district are phyllite and tuffaceous slate of the Shuangqiaoshan Group (Figure 3a,b). Biotite and actinolite hornfels are developed in the wall rocks surrounding the granodiorites (Figure 3c). The granodiorites are obliquely emplaced, and account for over 95 vol.% of igneous intrusions in this district. They show porphyritic texture in the peripheral and upper part of the intrusions (Figure 3d), and the center and lower portions grade into an equigranular texture (Figure 3e). Phenocrysts and groundmass have similar mineral composition to andesine, K-feldspar, quartz, hornblende, and biotite. Both the granodiorite and wall rocks are hydrothermally altered and mineralized (Figure 3f). LA-ICP-MS zircon U-Pb dating suggested that the granodiorite formed at $171 \pm 3$ Ma [20,38,63], contemporaneous with Cu-Mo mineralization (molybdenite Re-Os age of ~170 Ma [64]). The porphyry magmas are interpreted as a partial melt of Neoproterozoic subduction-modified lithosphere [20,38]. There is minor (<5 vol.%) post-diorite porphyry and aplite (Figure. 3g–i). The diorite truncates mineralized veins (Figure 3h,i), and has been dated at ca. 154 Ma by the zircon U-Pb method [65].
<figure><img src="image_5.png" /></figure>

**Figure 3.** Major lithologies (phyllite, slate, hornfel, and porphyries) and their spatial relation at the Tongchang porphyry Cu deposit. (a) an outcrop of phyllite; (b) a slate with pyrite stockworks and sericitic alteration halo; (c) a biotite hornfel; (d) a fresh granodiorite porphyry; (e) a fresh diorite porphyry; (f) a granodiorite porphyry crosscut by an anhydrite quartz vein; (g) a granodiorite porphyry truncating phyllite, both of which are altered by sericitic alteration; (h) a dioritic porphyry truncating slate, both of which are crosscut by a pyrite vein; (i) an altered porphyry truncating D-type pyrite vein (D.Vpd) hosted in the slate. The scale in (c) is a Chinese one-dime coin.

## 3.2. Hydrothermal Alteration

Typical hydrothermal alteration types are developed in the Tongchang deposit including potassic, propylitic, chlorite-sericite, and sericitic assemblages [66].

The potassic alteration is preserved only in the deep parts of the porphyry stock. At shallow levels, potassic alteration is largely obscured by chlorite-sericite overprints (Figure 4a). In the potassic altered granodiorite, porphyritic textures are preserved, but primary minerals are widely replaced by secondary K-feldspar, biotite, and iron oxides. Propylitic alteration is pervasive in the peripheral rocks. Rock textures are largely unaffected with carbonation and hydration reactions.
<figure><img src="image_5.png" /></figure>

**Figure 3.** Major lithologies (phyllite, slate, hornfel, and porphyries) and their spatial relation at the Tongchang porphyry Cu deposit. (a) an outcrop of phyllite; (b) a slate with pyrite stockworks and sericitic alteration halo; (c) a biotite hornfel; (d) a fresh granodiorite porphyry; (e) a fresh diorite porphyry; (f) a granodiorite porphyry crosscut by an anhydrite quartz vein; (g) a granodiorite porphyry truncating phyllite, both of which are altered by sericitic alteration; (h) a dioritic porphyry truncating slate, both of which are crosscut by a pyrite vein; (i) an altered porphyry truncating D-type pyrite vein (D.Vpd) hosted in the slate. The scale in (c) is a Chinese one-dime coin.

## 3.2. Hydrothermal Alteration

Typical hydrothermal alteration types are developed in the Tongchang deposit including potassic, propylitic, chlorite-sericite, and sericitic assemblages [66].

The potassic alteration is preserved only in the deep parts of the porphyry stock. At shallow levels, potassic alteration is largely obscured by chlorite-sericite overprints (Figure 4a). In the potassic altered granodiorite, porphyritic textures are preserved, but primary minerals are widely replaced by secondary K-feldspar, biotite, and iron oxides. Propylitic alteration is pervasive in the peripheral rocks. Rock textures are largely unaffected with carbonation and hydration reactions.
<figure><img src="image_6.png" /></figure>

**Figure 4.** Major types of hydrothermal alteration at the Tongchang porphyry Cu deposit. (a) Potassic alteration in the granodiorite porphyry; (b) Chlorite-sericite overprinting on potassic alteration in the granodiorite porphyry; (c) Chlorite-sericitic alteration in the granodiorite porphyry; (d) Sericitic overprinting on chlorite-sericitic alteration in the granodiorite porphyry; (e) Sericitic alteration with pyrite-dominated veins in the slate; (f) Propylitic alteration in the phyllite. Scale bars are 1 cm. The scale in (d) is a Chinese one-dime coin.

Moving away laterally from the granodiorite-wall rock contact, chlorite-sericite alterations overprint on potassic and propylitic alterations (Figure 4b,f). While rock textures are largely preserved, most previous minerals were converted to chlorite, sericite, chalcopyrite, rutile, quartz, and anhydrite (Figure 4d).

The spatial distribution of sericitic alterations is structurally controlled. It is mainly developed in the granodiorite-wall rock contacts and surrounding faults and fractures. It obliterated earlier rock textures and converted all mafic minerals and feldspars into muscovite, rutile, pyrite, and quartz (Figure 4c,e).

### 3.3. Hydrothermal Veinlets and Mineralization

Stockworks of veins and veinlets are widely developed alongside the hydrothermal alterations. A previous work recognized three vein types conformable to the typical A-B-D classification, as mentioned previously. [67] further distinguished four subtypes of A-type veins, seven subtypes of B-type veins, and three subtypes of D-type veins. The early A veins are mostly wavy quartz dominant veins with variable amounts of K-feldspar, biotite, and magnetite. The transitional B veins are mainly straight-walled chlorite and quartz veins with pyrite, chalcopyrite, molybdenite, and bornite, along the vein centerline and edges. The late D pyrite-dominant veins have variable amounts of chalcopyrite and quartz. A detailed vein petrography is provided in Section 4.1.

The district has a total resource of 1870 Mt ore at an average grade of 0.46% Cu. Individually, Tongchang has 5.2 Mt Cu at 0.45%, 0.128 Mt Mo at 0.01%, 215 t Au at 0.19 g/t and 1279 t Ag; Fujiawu has 2.57 Mt Cu at 0.5% and 0.168 Mt Mo at 0.03%; and Zhushahong has 0.6 Mt Cu at 0.42% [20]. Over 85% of the ore is localized in the chlorite-sericite and sericitic alteration zones, displaying a hollow cylinder shape (Figure 1d). Copper minerals are predominantly chalcopyrite (>90%), with lesser bornite, tennantite, and chalcocite. The molybdenum is mainly in molybdenite. Gold is recovered as native gold and electrum [68]. Sulfide occurrences are different in the chlorite-sericite and sericitic zones. In the former, copper sulfides and molybdenite are primarily contained in the B-type chalcopyrite veins and altered mafic minerals with high chalcopyrite to pyrite ratios (2–0.5). In the sericitic zones, copper sulfides occur primarily as inclusions in pyrite and occasionally as tennantite aggregates [64] with low chalcopyrite to pyrite ratios (<0.1). Molybdenite is
<figure><img src="image_6.png" /></figure>

**Figure 4.** Major types of hydrothermal alteration at the Tongchang porphyry Cu deposit. (a) Potassic alteration in the granodiorite porphyry; (b) Chlorite-sericite overprinting on potassic alteration in the granodiorite porphyry; (c) Chlorite-sericitic alteration in the granodiorite porphyry; (d) Sericitic overprinting on chlorite-sericitic alteration in the granodiorite porphyry; (e) Sericitic alteration with pyrite-dominated veins in the slate; (f) Propylitic alteration in the phyllite. Scale bars are 1 cm. The scale in (d) is a Chinese one-dime coin.

Moving away laterally from the granodiorite-wall rock contact, chlorite-sericite alterations overprint on potassic and propylitic alterations (Figure 4b,f). While rock textures are largely preserved, most previous minerals were converted to chlorite, sericite, chalcopyrite, rutile, quartz, and anhydrite (Figure 4d).

The spatial distribution of sericitic alterations is structurally controlled. It is mainly developed in the granodiorite-wall rock contacts and surrounding faults and fractures. It obliterated earlier rock textures and converted all mafic minerals and feldspars into muscovite, rutile, pyrite, and quartz (Figure 4c,e).

### 3.3. Hydrothermal Veinlets and Mineralization

Stockworks of veins and veinlets are widely developed alongside the hydrothermal alterations. A previous work recognized three vein types conformable to the typical A-B-D classification, as mentioned previously. [67] further distinguished four subtypes of A-type veins, seven subtypes of B-type veins, and three subtypes of D-type veins. The early A veins are mostly wavy quartz dominant veins with variable amounts of K-feldspar, biotite, and magnetite. The transitional B veins are mainly straight-walled chlorite and quartz veins with pyrite, chalcopyrite, molybdenite, and bornite, along the vein centerline and edges. The late D pyrite-dominant veins have variable amounts of chalcopyrite and quartz. A detailed vein petrography is provided in Section 4.1.

The district has a total resource of 1870 Mt ore at an average grade of 0.46% Cu. Individually, Tongchang has 5.2 Mt Cu at 0.45%, 0.128 Mt Mo at 0.01%, 215 t Au at 0.19 g/t and 1279 t Ag; Fujiawu has 2.57 Mt Cu at 0.5% and 0.168 Mt Mo at 0.03%; and Zhushahong has 0.6 Mt Cu at 0.42% [20]. Over 85% of the ore is localized in the chlorite-sericite and sericitic alteration zones, displaying a hollow cylinder shape (Figure 1d). Copper minerals are predominantly chalcopyrite (>90%), with lesser bornite, tennantite, and chalcocite. The molybdenum is mainly in molybdenite. Gold is recovered as native gold and electrum [68]. Sulfide occurrences are different in the chlorite-sericite and sericitic zones. In the former, copper sulfides and molybdenite are primarily contained in the B-type chalcopyrite veins and altered mafic minerals with high chalcopyrite to pyrite ratios (2–0.5). In the sericitic zones, copper sulfides occur primarily as inclusions in pyrite and occasionally as tennantite aggregates [64] with low chalcopyrite to pyrite ratios (<0.1). Molybdenite is
contained in D-type pyrite veins and altered wall rocks. Native Au, electrum and Au-rich pyrite are primarily hosted in the sericitic zone.

## 4. Samples and Methods

Sixteen representative rock samples were selected to represent different alteration and vein types. The sampling localities are marked in Figure 2 and Table 1, which include mining platforms (20 and 230 m) and drill cores of the Tongchang open pit (SC212), as well as drill cores (ZK0-2, ZK4-4, ZK6-3, ZK8-4, ZK821). Detailed descriptions of sample petrography are given in the Appendix A.
contained in D-type pyrite veins and altered wall rocks. Native Au, electrum and Au-rich pyrite are primarily hosted in the sericitic zone.

**4. Samples and Methods**

Sixteen representative rock samples were selected to represent different alteration and vein types. The sampling localities are marked in Figure 2 and Table 1, which include mining platforms (20 and 230 m) and drill cores of the Tongchang open pit (SC212), as well as drill cores (ZK0-2, ZK4-4, ZK6-3, ZK8-4, ZK821). Detailed descriptions of sample petrography are given in the Appendix A.
<table><caption>**Table 1.** A summary of sampling locality and petrography of the analyzed rock samples of the Tongchang porphyry Cu deposit.</caption><thead><tr><th>Sample NO.</th><th>Sampling Location</th><th>Vein type</th><th>Host Rock Alteration</th></tr></thead><tbody><tr><td>12LDX37</td><td>Drill hole SC212 171m</td><td>A.Vhq</td><td>The rock is significantly affected by chlorite-sericite alteration. Primary mafic minerals are replaced by chunks of chlorite, sericite, hematite, muscovite, and chalcopyrite. Feldspar phenocrysts are replaced by sericite. Quartz phenocrysts remain largely unaffected. Groundmass is replaced by fine-grained hematite and chalcopyrite. The rock is intensively crosscut by hematite quartz veins (Vhq), which are subsequently cut by chalcopyrite pyrite quartz veins and veinlets (Vcpq).</td></tr><tr><td>12LDX40</td><td>Drill hole SC212 175m</td><td></td><td>Feldspar phenocrysts are completely replaced by sericite. Primary mafic minerals are replaced by chlorite, rutile, and muscovite. Groundmass consists of muscovite, quartz, sericite, and chalcopyrite.</td></tr><tr><td>10DX172</td><td>Drill hole ZK8-4 933m</td><td></td><td>Plagioclase phenocrysts are partly (less than 50% of the surface) altered by sericite along cleavages and cracks. K-feldspar phenocrysts are completely replaced by sericite. Unidentified mineral pseudomorphs of inner sericite and outer chlorite, hematite and magnetite are present. Primary mafic minerals are replaced by chunks of small biotite, chlorite, hematite, and magnetite. Groundmass consists of sericite, quartz, biotite, hematite, and magnetite.</td></tr><tr><td>10DX197</td><td>Drill hole ZK8-4 777m</td><td>A.Vkq</td><td>K-feldspar phenocrysts are partly altered by muscovite and chlorite, and plagioclase are pseudomorphed by sericite and chlorite. Quartz grains are overgrown and enlarged. Primary biotites are pseudomorphed by muscovite, chlorite, rutile, and quartz. Numerous chunks of chlorite, sericite, muscovite, rutile, chalcopyrite, epidote, and calcite are present.</td></tr><tr><td>12DXF05</td><td>Open pit 230m platform</td><td></td><td>Feldspar phenocrysts are overgrown by K-feldspar, which are partly altered by sericite. Primary biotites are replaced by quartz, sericite, chalcopyrite, pyrite, and rutile. Quartz phenocrysts remain largely unaffected. Numerous chunks of chlorite are present. Groundmass consists of fine-grained quartz.</td></tr><tr><td>10DX168</td><td>Drill hole ZK8-4 943m</td><td></td><td>K-feldspar phenocrysts are pseudomorphed by sericite, and some anhedral K-feldspar grains are partly altered by sericite, chlorite, and epidote. Clusters of chlorites, sericite, anhydrite, epidote and molybdenite are present. Some quartz phenocrysts are overgrown, and others remain unaffected.</td></tr><tr><td>12DX500</td><td>Drill hole ZK821 620m</td><td>A.Vaq</td><td>K-feldspar phenocrysts are largely replaced by sericite, and plagioclase is slightly altered by sericite. Primary biotite remains largely unaffected, and some biotites are related by small, unoriented biotite, which are replaced by chlorite, sericite, quartz, hematite and magnetite. Groundmass consists of quartz, sericite, and chlorite.</td></tr><tr><td>10DX22</td><td>Drill hole ZK8-4 587m</td><td></td><td>The host rock is a diorite porphyry. Feldspars are completely replaced by sericite in the center and chlorite in the rim. Groundmass mainly consists of small biotite, sericite, and minor amounts of quartz.</td></tr><tr><td>10DX261</td><td>Open pit 20m platform</td><td>B.Vcpq</td><td>Feldspar phenocrysts are completely replaced by sericite and muscovite. Primary biotites are pseudomorphed by chlorite, rutile, sericite and chalcopyrite. The rock is intensively cut by chlorite-muscovite-chalcopyrite-pyrite veins.</td></tr></tbody></table>
<table><caption>**Table 1.** A summary of sampling locality and petrography of the analyzed rock samples of the Tongchang porphyry Cu deposit.</caption><thead><tr><th>Sample NO.</th><th>Sampling Location</th><th>Vein type</th><th>Host Rock Alteration</th></tr></thead><tbody><tr><td>12LDX37</td><td>Drill hole SC212 171m</td><td>A.Vhq</td><td>The rock is significantly affected by chlorite-sericite alteration. Primary mafic minerals are replaced by chunks of chlorite, sericite, hematite, muscovite, and chalcopyrite. Feldspar phenocrysts are replaced by sericite. Quartz phenocrysts remain largely unaffected. Groundmass is replaced by fine-grained hematite and chalcopyrite. The rock is intensively crosscut by hematite quartz veins (Vhq), which are subsequently cut by chalcopyrite pyrite quartz veins and veinlets (Vcpq).</td></tr><tr><td>12LDX40</td><td>Drill hole SC212 175m</td><td></td><td>Feldspar phenocrysts are completely replaced by sericite. Primary mafic minerals are replaced by chlorite, rutile, and muscovite. Groundmass consists of muscovite, quartz, sericite, and chalcopyrite.</td></tr><tr><td>10DX172</td><td>Drill hole ZK8-4 933m</td><td></td><td>Plagioclase phenocrysts are partly (less than 50% of the surface) altered by sericite along cleavages and cracks. K-feldspar phenocrysts are completely replaced by sericite. Unidentified mineral pseudomorphs of inner sericite and outer chlorite, hematite and magnetite are present. Primary mafic minerals are replaced by chunks of small biotite, chlorite, hematite, and magnetite. Groundmass consists of sericite, quartz, biotite, hematite, and magnetite.</td></tr><tr><td>10DX197</td><td>Drill hole ZK8-4 777m</td><td>A.Vkq</td><td>K-feldspar phenocrysts are partly altered by muscovite and chlorite, and plagioclase are pseudomorphed by sericite and chlorite. Quartz grains are overgrown and enlarged. Primary biotites are pseudomorphed by muscovite, chlorite, rutile, and quartz. Numerous chunks of chlorite, sericite, muscovite, rutile, chalcopyrite, epidote, and calcite are present.</td></tr><tr><td>12DXF05</td><td>Open pit 230m platform</td><td></td><td>Feldspar phenocrysts are overgrown by K-feldspar, which are partly altered by sericite. Primary biotites are replaced by quartz, sericite, chalcopyrite, pyrite, and rutile. Quartz phenocrysts remain largely unaffected. Numerous chunks of chlorite are present. Groundmass consists of fine-grained quartz.</td></tr><tr><td>10DX168</td><td>Drill hole ZK8-4 943m</td><td></td><td>K-feldspar phenocrysts are pseudomorphed by sericite, and some anhedral K-feldspar grains are partly altered by sericite, chlorite, and epidote. Clusters of chlorites, sericite, anhydrite, epidote and molybdenite are present. Some quartz phenocrysts are overgrown, and others remain unaffected.</td></tr><tr><td>12DX500</td><td>Drill hole ZK821 620m</td><td>A.Vaq</td><td>K-feldspar phenocrysts are largely replaced by sericite, and plagioclase is slightly altered by sericite. Primary biotite remains largely unaffected, and some biotites are related by small, unoriented biotite, which are replaced by chlorite, sericite, quartz, hematite and magnetite. Groundmass consists of quartz, sericite, and chlorite.</td></tr><tr><td>10DX22</td><td>Drill hole ZK8-4 587m</td><td></td><td>The host rock is a diorite porphyry. Feldspars are completely replaced by sericite in the center and chlorite in the rim. Groundmass mainly consists of small biotite, sericite, and minor amounts of quartz.</td></tr><tr><td>10DX261</td><td>Open pit 20m platform</td><td>B.Vcpq</td><td>Feldspar phenocrysts are completely replaced by sericite and muscovite. Primary biotites are pseudomorphed by chlorite, rutile, sericite and chalcopyrite. The rock is intensively cut by chlorite-muscovite-chalcopyrite-pyrite veins.</td></tr></tbody></table>
<table><tr><td>12DX328</td><td>Drill hole ZK821 499m</td><td>B.V<sub>macpq</sub></td><td>The center of feldspar phenocryst is replaced by chlorite while rim is replaced by sericite. Primary mafic minerals are replaced by chlorite, rutile, chalcopyrite, hematite, and magnetite. Aggregations of chlorite-rutile- magnetite, chlorite-chalcopyrite-rutile-anhydrite are present. Groundmass consists of quartz, anhydrite, rutile, and muscovite. Molybdenite occurs in both alteration and vein.</td></tr><tr><td>10DX164</td><td>Drill hole ZK8-4 952m</td><td>D.V<sub>mqp</sub></td><td>Feldspar phenocrysts are pseudomorphed by sericite. Mafic mineral pseudomorphs are not common. Where observed, they consist of chlorite and pyrite. The rock is intensely silicified. Quartz in the groundmass is medium-sized, intergrowing with abundant muscovite and chlorite. Sulfides are dominated by pyrite and occur as aggregations and bands.</td></tr><tr><td>10DX220</td><td>Drill hole ZK8-4 601m</td><td></td><td>The immediate host rock consists of strong Sericitic alteration halos of the molybdenite quartz pyrite vein. In the halo, primary minerals except quartz are completely replaced by large muscovite, rutile, quartz, and pyrite. No mineral pseudomorphs are eliminated. Groundmass consists of fine-grained quartz and large muscovite.</td></tr><tr><td>10DX140</td><td>Drill hole ZK0-2 337m</td><td></td><td>The rock is a sericitic altered phyllite, consisting of oriented sericite, quartz, pyrite, and rutile.</td></tr><tr><td>10DX145</td><td>Drill hole ZK4-4 410m</td><td></td><td>It is a sericitic altered phyllite, consisting of oriented sericite, quartz, pyrite, and rutile.</td></tr><tr><td>10DX158</td><td>Drill hole ZK6-3 1067m</td><td>D.V<sub>pd</sub></td><td>It is a slate with Propylitic alteration, consisting of randomly distributed chlorite, sericite, and quartz.</td></tr><tr><td>10DX201</td><td>Drill hole ZK8-4 738m</td><td></td><td>It is a breccia consisting of pyrite, quartz, and carbonate.</td></tr></table>
<table><tr><td>12DX328</td><td>Drill hole ZK821 499m</td><td>B.V<sub>macpq</sub></td><td>The center of feldspar phenocryst is replaced by chlorite while rim is replaced by sericite. Primary mafic minerals are replaced by chlorite, rutile, chalcopyrite, hematite, and magnetite. Aggregations of chlorite-rutile- magnetite, chlorite-chalcopyrite-rutile-anhydrite are present. Groundmass consists of quartz, anhydrite, rutile, and muscovite. Molybdenite occurs in both alteration and vein.</td></tr><tr><td>10DX164</td><td>Drill hole ZK8-4 952m</td><td>D.V<sub>mqp</sub></td><td>Feldspar phenocrysts are pseudomorphed by sericite. Mafic mineral pseudomorphs are not common. Where observed, they consist of chlorite and pyrite. The rock is intensely silicified. Quartz in the groundmass is medium-sized, intergrowing with abundant muscovite and chlorite. Sulfides are dominated by pyrite and occur as aggregations and bands.</td></tr><tr><td>10DX220</td><td>Drill hole ZK8-4 601m</td><td></td><td>The immediate host rock consists of strong Sericitic alteration halos of the molybdenite quartz pyrite vein. In the halo, primary minerals except quartz are completely replaced by large muscovite, rutile, quartz, and pyrite. No mineral pseudomorphs are eliminated. Groundmass consists of fine-grained quartz and large muscovite.</td></tr><tr><td>10DX140</td><td>Drill hole ZK0-2 337m</td><td></td><td>The rock is a sericitic altered phyllite, consisting of oriented sericite, quartz, pyrite, and rutile.</td></tr><tr><td>10DX145</td><td>Drill hole ZK4-4 410m</td><td></td><td>It is a sericitic altered phyllite, consisting of oriented sericite, quartz, pyrite, and rutile.</td></tr><tr><td>10DX158</td><td>Drill hole ZK6-3 1067m</td><td>D.V<sub>pd</sub></td><td>It is a slate with Propylitic alteration, consisting of randomly distributed chlorite, sericite, and quartz.</td></tr><tr><td>10DX201</td><td>Drill hole ZK8-4 738m</td><td></td><td>It is a breccia consisting of pyrite, quartz, and carbonate.</td></tr></table>
## 4.1. Vein Petrography

Three subtypes of A-type veins have been selected: hematite-quartz (A.Vhq), K-feldspar-quartz (A.Vkq), and anhydrite-quartz (A.Vaq). In the abbreviation, A denotes A-type, and the subscripts denote vein minerals in increasing mounts from left to right. The same abbreviation rule is used for all vein types.

A.Vhq veins have irregular vein boundaries without discernible alteration halos. They consist of about 95% quartz and 5% hematite (Figure 5a). They are commonly crosscut and reopened by chlorite-sericite-chalcopyrite-magnetite veins. A.Vkq veins consist of about 80–90% quartz and 10–20% K-feldspar, and are commonly enveloped by potassic halos (Figure 5b). Similarly, they are commonly crosscut and reopened by veinlets of chalcopyrite, muscovite, pyrite, and carbonate. A.Vaq veins consist of about 70% quartz, 20–30% anhydrite and variable amounts of pyrite, chalcopyrite, chlorite, carbonate, rutile, molybdenite, apatite and epidote (Figure 5c,d). They are commonly sandwiched by weak potassic halos. No crosscutting relationships have been observed between these three vein types.

<figure><img src="image_7.png" /><figcaption>**Figure 5.** Hydrothermal vein types recognized in the Tongchang porphyry Cu deposit. (a) An A-type hematite quartz vein in the granodiorite porphyry (A.Vhq), crosscut by a B-type chalcopyrite pyrite quartz vein (B.Vcpq); (b) An A-type K-feldspar quartz vein in the granodiorite porphyry (A.Vkq); (c,d) A-type anhydrite quartz veins in the granodiorite porphyry (A.Vaq); (e) A B-type chalcopyrite pyrite quartz vein in the granodiorite porphyry (B.Vcpq); (f) A B-type molybdenite anhydrite chalcopyrite pyrite quartz vein in the granodiorite porphyry (B.Vmacpq) with chlorite-sericite halos; (g) A D-type quartz pyrite vein in the granodiorite porphyry with sericitic halo (D.Vqp); (h) A D-type pyrite-dominated veins (D.Vpd) in phyllite.</figcaption></figure>

Two B subtype veins have been selected, including chalcopyrite-pyrite-quartz (B.Vcpq) and molybdenite-anhydrite-chalcopyrite-pyrite quartz vein (B.Vmacpq). They are characterized by centerlines of sulfides and straight vein boundaries without alteration halos. B.Vcpq veins consist of about 70–90% quartz and 10–30% sulfides, with variable pyrite to chalcopyrite ratios (Figure 5e). B.Vmacpq veins differ from B.Vcpq veins with additional molybdenite and anhydrite in the vein and chloritic alteration halos. They commonly consist of about 70% quartz, 10% pyrite, 5–10% chalcopyrite, 5% anhydrite and minor amounts of molybdenite (Figure 5f). B.Vcpq and B.Vmacpq crosscut B.Vhq veins but no other crosscutting relations have been observed between B subtypes.
## 4.1. Vein Petrography

Three subtypes of A-type veins have been selected: hematite-quartz (A.Vhq), K-feldspar-quartz (A.Vkq), and anhydrite-quartz (A.Vaq). In the abbreviation, A denotes A-type, and the subscripts denote vein minerals in increasing amounts from left to right. The same abbreviation rule is used for all vein types.

A.Vhq veins have irregular vein boundaries without discernible alteration halos. They consist of about 95% quartz and 5% hematite (Figure 5a). They are commonly crosscut and reopened by chlorite-sericite-chalcopyrite-magnetite veins. A.Vkq veins consist of about 80–90% quartz and 10–20% K-feldspar, and are commonly enveloped by potassic halos (Figure 5b). Similarly, they are commonly crosscut and reopened by veinlets of chalcopyrite, muscovite, pyrite, and carbonate. A.Vaq veins consist of about 70% quartz, 20–30% anhydrite and variable amounts of pyrite, chalcopyrite, chlorite, carbonate, rutile, molybdenite, apatite and epidote (Figure 5c,d). They are commonly sandwiched by weak potassic halos. No crosscutting relationships have been observed between these three vein types.

<figure><img src="image_7.png" /><figcaption>**Figure 5.** Hydrothermal vein types recognized in the Tongchang porphyry Cu deposit. (a) An A-type hematite quartz vein in the granodiorite porphyry (A.Vhq), crosscut by a B-type chalcopyrite pyrite quartz vein (B.Vcpq); (b) An A-type K-feldspar quartz vein in the granodiorite porphyry (A.Vkq); (c,d) A-type anhydrite quartz veins in the granodiorite porphyry (A.Vaq); (e) A B-type chalcopyrite pyrite quartz vein in the granodiorite porphyry (B.Vcpq); (f) A B-type molybdenite anhydrite chalcopyrite pyrite quartz vein in the granodiorite porphyry (B.Vmacpq) with chlorite-sericite halos; (g) A D-type quartz pyrite vein in the granodiorite porphyry with sericitic halo (D.Vqp); (h) A D-type pyrite-dominated veins (D.Vpd) in phyllite.</figcaption></figure>

Two B subtype veins have been selected, including chalcopyrite-pyrite-quartz (B.Vcpq) and molybdenite-anhydrite-chalcopyrite-pyrite quartz vein (B.Vmacpq). They are characterized by centerlines of sulfides and straight vein boundaries without alteration halos. B.Vcpq veins consist of about 70–90% quartz and 10–30% sulfides, with variable pyrite to chalcopyrite ratios (Figure 5e). B.Vmacpq veins differ from B.Vcpq veins with additional molybdenite and anhydrite in the vein and chloritic alteration halos. They commonly consist of about 70% quartz, 10% pyrite, 5–10% chalcopyrite, 5% anhydrite and minor amounts of molybdenite (Figure 5f). B.Vcpq and B.Vmacpq crosscut B.Vhq veins but no other crosscutting relations have been observed between B subtypes.
Two D subtype veins have been selected including molybdenite-quartz-pyrite (D.V<sub>mqp</sub>) and pyrite-dominant (D.V<sub>pd</sub>). D.V<sub>mqp</sub> veins containing about 70–80% pyrite and 15–20% quartz and 5% molybdenite, bordered by centimeter-wide sericitic alteration halos (Figure 5g). D.V<sub>mqp</sub> veins are crosscut by D.V<sub>pd</sub> veins, but their relationships with other vein types is unclear. D.V<sub>pd</sub> veins are dominated by pyrite (>95%) with minor amounts of quartz (<5%), and are commonly bordered by sericitic alteration halos (Figure 5h). D.V<sub>pd</sub> veins usually crosscut A.V<sub>hq</sub>, B.V<sub>cpq</sub>, and D.V<sub>mqp</sub> veins.

## 4.2. Analytical Methods

300 µm-thick sections were made by conventional cutting, grinding, and polishing. Mineral textures and parageneses were studied with petrographic microscopes and scanning electron microscopes (SEM) equipped with secondary electron (SE), backscattered electron (BSE), cathodoluminescence (CL), and energy dispersive spectroscopy (EDS) detectors. A total of 774 grey-scale CL, 579 color CL, 782 BSE high-resolution images, and 42 X-ray maps were taken. Trace element concentrations in different generations of quartz were measured in situ by LA-ICP-MS. Overall, 656 analyses for quartz from 16 samples were made. After all analyses, the actual ablation spots were confirmed by new CL imagery.

### 4.2.1. SEM-CL Microscopy

Greyscale CL imagery for anhydrite and quartz were firstly obtained on a Tescan Vega3 SEM equipped with a Centaurus CL detector and a photomultiplier at the Western Washington University. The accelerating voltage was 15 kV, and the probe current was about 10 nA for both quartz and anhydrite. The photomultiplier had a spectral range from ~300 nm to ~600 nm. A later CL study was carried out at the Institute of Geology and Geophysics, Chinese Academy of Sciences (IGGCAS), with a Nova NanoSEM 450 SEM equipped with a Gatan MonoCL4 panchromatic detector. An acceleration voltage of 15 kV and beam current of 9–12 nA were used.

Color CL images of quartz and anhydrite were collected using a Tescan Vega3 SEM equipped with a Gatan ChromaCL2 multichromatic detector at the GeoRessources Lab, CNRS (UMR7359), Université de Lorraine. An acceleration voltage of 15 kV and beam current of ~10 nA was used. The CL detector records spectra in ranges of red, green, and blue, and produces an RGB image. A dwell time of 300 µs was set for each pixel. During a separate session aiming to test the lifespan of luminescence, images were taken after the samples were exposed to electron beams for a certain amount of time.

### 4.2.2. In-Situ LA-ICP-MS Trace Elements

Trace elements in quartz were first measured with an Agilent 7500 ce ICP-MS coupled with a NewWave 213 nm Nd:YAG solid state laser ablation system at WWU. A laser fluence of 15 to 20 J/cm², a repetition rate of 10 Hz, and a spot size of 65 µm were used. Helium was used as a carrier gas and mixed with make-up argon gas before entering the ICP torch. The Octupole Reaction System (ORS) was operated in hydrogen reaction mode (H₂ flow rate of 2 mL/min) to increase sensitivity. Oxide production was monitored with ¹³²Th¹⁶O/¹³²Th ratios, which were always less than 0.2%. Twenty-two masses were monitored: ⁷Li, ⁹Be, ¹¹B, ²³Na, ²⁷Al, ²⁹Si, ³⁰Si, ³¹P, ³⁹K, ⁴³Ca, ⁴⁹Ti, ⁵⁵Mn, ⁵⁶Fe, ⁶³Cu, ⁷¹Ga, ⁷⁴Ge, ⁷⁵As, ⁸⁸Sr, ¹¹⁸Sn, ¹²¹Sb, ¹³⁷Ba, and ²⁰⁸Pb. The dwelling time for ⁴⁹Ti was 0.1 s, and it was 0.01–0.03 s for the other masses. About 30 s of gas blank was collected as the baseline, which was followed by 60 s of data acquisition with laser ablation. Instrument performance was checked by a rough on-the-fly data reduction with the GLITTER program. Data were reduced with care later on using GLITTER. ³⁰Si was used as the internal standard using stoichiometric values. NIST 610 glass was used as an external standard, with reference values from [69]. A natural quartz standard (QZ7 [70]) and a synthetic quartz with a known chemical composition was used as quality controls. Results for QZ7 were within the range of
Two D subtype veins have been selected including molybdenite-quartz-pyrite (D.Vmqp) and pyrite-dominant (D.Vpd). D.Vmqp veins containing about 70–80% pyrite and 15–20% quartz and 5% molybdenite, bordered by centimeter-wide sericitic alteration halos (Figure 5g). D.Vmqp veins are crosscut by D.Vpd veins, but their relationships with other vein types is unclear. D.Vpd veins are dominated by pyrite (>95%) with minor amounts of quartz (<5%), and are commonly bordered by sericitic alteration halos (Figure 5h). D.Vpd veins usually crosscut A.Vhq, B.Vcpq, and D.Vmqp veins.

## 4.2. Analytical Methods

300 µm-thick sections were made by conventional cutting, grinding, and polishing. Mineral textures and parageneses were studied with petrographic microscopes and scanning electron microscopes (SEM) equipped with secondary electron (SE), backscattered electron (BSE), cathodoluminescence (CL), and energy dispersive spectroscopy (EDS) detectors. A total of 774 grey-scale CL, 579 color CL, 782 BSE high-resolution images, and 42 X-ray maps were taken. Trace element concentrations in different generations of quartz were measured in situ by LA-ICP-MS. Overall, 656 analyses for quartz from 16 samples were made. After all analyses, the actual ablation spots were confirmed by new CL imagery.

### 4.2.1. SEM-CL Microscopy

Greyscale CL imagery for anhydrite and quartz were firstly obtained on a Tescan Vega3 SEM equipped with a Centaurus CL detector and a photomultiplier at the Western Washington University. The accelerating voltage was 15 kV, and the probe current was about 10 nA for both quartz and anhydrite. The photomultiplier had a spectral range from ~300 nm to ~600 nm. A later CL study was carried out at the Institute of Geology and Geophysics, Chinese Academy of Sciences (IGGCAS), with a Nova NanoSEM 450 SEM equipped with a Gatan MonoCL4 panchromatic detector. An acceleration voltage of 15 kV and beam current of 9–12 nA were used.

Color CL images of quartz and anhydrite were collected using a Tescan Vega3 SEM equipped with a Gatan ChromaCL2 multichromatic detector at the GeoRessources Lab, CNRS (UMR7359), Université de Lorraine. An acceleration voltage of 15 kV and beam current of ~10 nA was used. The CL detector records spectra in ranges of red, green, and blue, and produces an RGB image. A dwell time of 300 µs was set for each pixel. During a separate session aiming to test the lifespan of luminescence, images were taken after the samples were exposed to electron beams for a certain amount of time.

### 4.2.2. In-Situ LA-ICP-MS Trace Elements

Trace elements in quartz were first measured with an Agilent 7500 ce ICP-MS coupled with a NewWave 213 nm Nd:YAG solid state laser ablation system at WWU. A laser fluence of 15 to 20 J/cm², a repetition rate of 10 Hz, and a spot size of 65 µm were used. Helium was used as a carrier gas and mixed with make-up argon gas before entering the ICP torch. The Octupole Reaction System (ORS) was operated in hydrogen reaction mode (H₂ flow rate of 2 mL/min) to increase sensitivity. Oxide production was monitored with ¹³²Th¹⁶O/¹³²Th ratios, which were always less than 0.2%. Twenty-two masses were monitored: ⁷Li, ⁹Be, ¹¹B, ²³Na, ²⁷Al, ²⁹Si, ³⁰Si, ³¹P, ³⁹K, ⁴³Ca, ⁴⁹Ti, ⁵⁵Mn, ⁵⁶Fe, ⁶³Cu, ⁷¹Ga, ⁷⁴Ge, ⁷⁵As, ⁸⁸Sr, ¹¹⁸Sn, ¹²¹Sb, ¹³⁷Ba, and ²⁰⁸Pb. The dwelling time for ⁴⁹Ti was 0.1 s, and it was 0.01–0.03 s for the other masses. About 30 s of gas blank was collected as the baseline, which was followed by 60 s of data acquisition with laser ablation. Instrument performance was checked by a rough on-the-fly data reduction with the GLITTER program. Data were reduced with care later on using GLITTER. ³⁰Si was used as the internal standard using stoichiometric values. NIST 610 glass was used as an external standard, with reference values from [69]. A natural quartz standard (QZ7 [70]) and a synthetic quartz with a known chemical composition was used as quality controls. Results for QZ7 were within the range of
recommended values for all elements except lower Al values. A correction factor was obtained by dividing the recommended value by measured values of Qz7 (ranging from 0.51 to 0.76, Table 4), which was applied to unknowns of the same analytical session. Additional analyses were made with an Agilent 7900 ICP-MS equipped with a MICRO/Las Pro 193 nm ArF excimer laser ablation system at the Institute of Geochemistry of the Chinese Academy of Sciences (IGCAS). A repetition rate of 10 Hz and an energy density of 10 J/cm² were used. Spot size of the laser beam was 44 µm. NIST 610 glass was used as an external standard and analyzed twice every 10 analyses. An internal standard-independent calibration strategy, implemented in the ICPMSDataCal program, was used for quantification [71]. NIST 612, GSE-1G, and Qz7 were analyzed as quality controls. Analytical uncertainties of most elements for both setups were around 5–10% (1σ).

Although every effort was taken to avoid mineral and fluid inclusions, the influence of sub-microscopic inclusions was inevitable. During data reduction, abnormal spikes and bumps were filtered and excluded from integration. Even so, values of Na, K, Ca, Al, Mn, Fe, Cu, Zn, Sr, As, and Pb were too high to be real. Co-variations in Na-K-Al, Ca-Sr, Fe-Cu, Ca-Pb, K-Ca-Al, Cu-As, and Fe-Mn was interpreted to be the result of feldspar, carbonate, chalcopyrite/pyrite, tennantite, mica, and fluid inclusions, and were used as the basis to discard those values.

### 4.2.3. Fluid Inclusion Microthermometry

Fluid inclusions were classified as primary, secondary and pseudosecondary, following the principles of [72]. Phase transition temperatures were measured on a Linkam THMS 600 cooling/heating stage at the GeoRessources Lab of the Université de Lorraine. The stage was calibrated against the melting point of solid CO₂ (–56.6 °C) and ice (0 °C), and a homogenization temperature (165 °C) of well-characterized natural fluid inclusions. The heating rate varied between 0.2 and 10 °C/min. When fluid inclusions approached the phase transition, the rate was lowered to 0.2–0.5 °C/min. Fluid salinity, density and isochores were calculated using the HokieFlincs_H₂O-NaCl program [73].

## 5. Results

### 5.1. SEM-CL Imaging

Quartz growth sequencing was based on CL micro textures and vein crosscutting relations. The earliest quartz generation (Qz1, Figure 6a), most common in the A.Vhq, B.Vcpq, and B.Vmacpq veins, was characterized by variable grain sizes and straight grain boundaries. The grains commonly show undulose extinction under polarized light. They exhibit mottled CL with faint zoning, and abundant microfractures that are filled with CL-dark “splatters” and “cobwebs” (Figure 6a).
recommended values for all elements except lower Al values. A correction factor was obtained by dividing the recommended value by measured values of Qz7 (ranging from 0.51 to 0.76, Table 4), which was applied to unknowns of the same analytical session. Additional analyses were made with an Agilent 7900 ICP-MS equipped with a MICRO/Las Pro 193 nm ArF excimer laser ablation system at the Institute of Geochemistry of the Chinese Academy of Sciences (IGCAS). A repetition rate of 10 Hz and an energy density of 10 J/cm² were used. Spot size of the laser beam was 44 µm. NIST 610 glass was used as an external standard and analyzed twice every 10 analyses. An internal standard-independent calibration strategy, implemented in the ICPMSDataCal program, was used for quantification [71]. NIST 612, GSE-1G, and Qz7 were analyzed as quality controls. Analytical uncertainties of most elements for both setups were around 5–10% (1σ).

Although every effort was taken to avoid mineral and fluid inclusions, the influence of sub-microscopic inclusions was inevitable. During data reduction, abnormal spikes and bumps were filtered and excluded from integration. Even so, values of Na, K, Ca, Al, Mn, Fe, Cu, Zn, Sr, As, and Pb were too high to be real. Co-variations in Na-K-Al, Ca-Sr, Fe-Cu, Ca-Pb, K-Ca-Al, Cu-As, and Fe-Mn was interpreted to be the result of feldspar, carbonate, chalcopyrite/pyrite, tennantite, mica, and fluid inclusions, and were used as the basis to discard those values.

### 4.2.3. Fluid Inclusion Microthermometry

Fluid inclusions were classified as primary, secondary and pseudosecondary, following the principles of [72]. Phase transition temperatures were measured on a Linkam THMS 600 cooling/heating stage at the GeoRessources Lab of the Université de Lorraine. The stage was calibrated against the melting point of solid CO₂ (–56.6 °C) and ice (0 °C), and a homogenization temperature (165 °C) of well-characterized natural fluid inclusions. The heating rate varied between 0.2 and 10 °C/min. When fluid inclusions approached the phase transition, the rate was lowered to 0.2–0.5 °C/min. Fluid salinity, density and isochores were calculated using the HokieFlincs_H₂O-NaCl program [73].

## 5. Results

### 5.1. SEM-CL Imaging

Quartz growth sequencing was based on CL micro textures and vein crosscutting relations. The earliest quartz generation (Qz1, Figure 6a), most common in the A.Vhq, B.Vcpq, and B.Vmacpq veins, was characterized by variable grain sizes and straight grain boundaries. The grains commonly show undulose extinction under polarized light. They exhibit mottled CL with faint zoning, and abundant microfractures that are filled with CL-dark “splatters” and “cobwebs” (Figure 6a).
<figure><img src="image_8.png" /></figure>

**Figure 6.** CL micro textures of quartz at the Tongchang porphyry Cu deposit. (a) The earliest CL-homogeneous quartz (Qz1) reopened by later veinlet; (b,c) The second generation (Qz2a and Qz2b) that shows dark blue CL with faint zoning. Also shown are three generations of anhydrite (purple); (d) The third generation of quartz (Qz3a and Qz3b) resorbing and overgrowing on early Qz2b. Note that the Qz3a has lower CL intensity than Qz3b does; (e) Qz3b directly overgrown on Qz2b, showing conformable contact with the surrounding pyrite; (f) Qz2 and Qz3 displayed blue CL with different intensities; (g,h) Coprecipitation of CL-dark Qz4 (overgrown blue-CL Qz3b) and Anh4 (cementing purple-CL Anh2 breccia); (i) Qz5a and Qz5b overgrew on Qz3b. (j) Qz5a fill in fractures in Qz3a. Note that Qz5a has lower CL than Qz5b; (k) CL-homogeneous Qz6a and CL-oscillatory Qz6b. Note that Qz6b has bright CL. (l) Qz6a shows red CL, whereas Qz6b shows bright blue C. Scale bars are 300 µm.

The second quartz generation of (Qz2), common in A.V<sub>kq</sub>, A.V<sub>aq</sub>, B.V<sub>cpq</sub>, B.V<sub>macpq</sub>, D.V<sub>pq</sub>, and D.V<sub>pd</sub> comprises anhedral grains with contrast sizes and irregular boundaries filled with CL-dark quartz. Qz2 grains are further divided into larger Qz2a grains that have concentric CL zoning and smaller Qz2b grains that show mottled CL (Figure 6b). The contacts between Qz2a and Qz2b can be both transitional and crosscutting. They form discrete layers in most samples. They also contain “splatters” and “cobwebs”. Under color CL, both grains show long-lived blue, with lower intensity for Qz2b (Figure 6c). Qz2 grains truncate Q1 locally, suggesting a later deposition.

The third generation of quartz (Qz3), common in the A.V<sub>kq</sub>, B.V<sub>macpq</sub>, D.V<sub>mpq</sub>, D.V<sub>pq</sub>, and D.V<sub>pd</sub> veins, comprises a CL-dark core (Qz3a) and an overgrowth with oscillatory zoning (Qz3b) (Figure 6d). Some Qz3 grains contain a relict Qz1/Qz2 core overgrown either by Qz3a or Qz3b (Figure 6e). They also show long-lived blue CL (Figure 6f).

The fourth generation of quartz (Qz4), mainly observed in the A.V<sub>aq</sub>, B.V<sub>cpq</sub>, and B.V<sub>macpq</sub> veins, is low in abundance. The Qz4 grains show dark, red CL and occur as thin rims or aggregates coating earlier quartz (Figure 6e,g,h). Qz4 crosscuts Qz3b grains locally.

The fifth generation of quartz (Qz5) commonly consists of a CL-dark core (Qz5a) and oscillatory overgrowth (Qz5b) (Figure 6i). They are observed in the D.V<sub>mpq</sub>, D.V<sub>pq</sub>, and
<figure><img src="image_8.png" /></figure>

**Figure 6.** CL micro textures of quartz at the Tongchang porphyry Cu deposit. (a) The earliest CL-homogeneous quartz (Qz1) reopened by later veinlet; (b,c) The second generation (Qz2a and Qz2b) that shows dark blue CL with faint zoning. Also shown are three generations of anhydrite (purple); (d) The third generation of quartz (Qz3a and Qz3b) resorbing and overgrowing on early Qz2b. Note that the Qz3a has lower CL intensity than Qz3b does; (e) Qz3b directly overgrown on Qz2b, showing conformable contact with the surrounding pyrite; (f) Qz2 and Qz3 displayed blue CL with different intensities; (g,h) Coprecipitation of CL-dark Qz4 (overgrown blue-CL Qz3b) and Anh4 (cementing purple-CL Anh2 breccia); (i) Qz5a and Qz5b overgrew on Qz3b. (j) Qz5a fill in fractures in Qz3a. Note that Qz5a has lower CL than Qz5b; (k) CL-homogeneous Qz6a and CL-oscillatory Qz6b. Note that Qz6b has bright CL. (l) Qz6a shows red CL, whereas Qz6b shows bright blue C. Scale bars are 300 µm.

The second quartz generation of (Qz2), common in A.V<sub>kq</sub>, A.V<sub>aq</sub>, B.V<sub>cpq</sub>, B.V<sub>macpq</sub>, D.V<sub>pq</sub>, and D.V<sub>pd</sub> comprises anhedral grains with contrast sizes and irregular boundaries filled with CL-dark quartz. Qz2 grains are further divided into larger Qz2a grains that have concentric CL zoning and smaller Qz2b grains that show mottled CL (Figure 6b). The contacts between Qz2a and Qz2b can be both transitional and crosscutting. They form discrete layers in most samples. They also contain “splatters” and “cobwebs”. Under color CL, both grains show long-lived blue, with lower intensity for Qz2b (Figure 6c). Qz2 grains truncate Q1 locally, suggesting a later deposition.

The third generation of quartz (Qz3), common in the A.V<sub>kq</sub>, B.V<sub>macpq</sub>, D.V<sub>mpq</sub>, D.V<sub>pq</sub>, and D.V<sub>pd</sub> veins, comprises a CL-dark core (Qz3a) and an overgrowth with oscillatory zoning (Qz3b) (Figure 6d). Some Qz3 grains contain a relict Qz1/Qz2 core overgrown either by Qz3a or Qz3b (Figure 6e). They also show long-lived blue CL (Figure 6f).

The fourth generation of quartz (Qz4), mainly observed in the A.V<sub>aq</sub>, B.V<sub>cpq</sub>, and B.V<sub>macpq</sub> veins, is low in abundance. The Qz4 grains show dark, red CL and occur as thin rims or aggregates coating earlier quartz (Figure 6e,g,h). Qz4 crosscuts Qz3b grains locally.

The fifth generation of quartz (Qz5) commonly consists of a CL-dark core (Qz5a) and oscillatory overgrowth (Qz5b) (Figure 6i). They are observed in the D.V<sub>mpq</sub>, D.V<sub>pq</sub>, and
D.Vpd veins, and are intimately associated with pyrite. Locally, they occur as dark bands crosscutting or filling the interstitial space of earlier quartz (Figure 6j).

The latest generation of quartz (Qz6) comprises a CL-dark to grey interior (Qz6a) and a very bright-CL exterior (Qz6b) (Figure 6k). They were observed in the A.Vaq, D.Vpq, and D.Vpd. Qz6a exhibited an oscillation of red and blue CL, whereas Qz6b displayed a bright yellowish blue (Figure 6l).

Four generations of anhydrite have been identified. The first generation of anhydrite (Anh1) exhibited bright, homogeneous to patchy CL (Figure 7a). They are subdivided to Anh1a and Anh1b according to CL intensity. Anh1a grains have higher CL intensity and irregular boundaries (Figure 7a) relative to Anh1b grains that are commonly overgrown, recrystallized, or crosscut by later anhydrites.

<figure><img src="image_9.png" /></figure>

**Figure 7.** Cathodoluminescence (CL) micro textures of vein anhydrite at the Tongchang porphyry Cu deposit. (a) The first generation of anhydrite (Anh1), rimed and surrounded by CL-oscillatory Anh2, coexisting with pyrite and quartz; (b) Anh2a showing "wavy" oscillatory zoning; (c) A cluster of euhedral Anh3a and Anh3b grains, with Anh3a showing oscillatory zoning, whereas Anh3b showed homogeneous CL; (d,e) CL-dark Anh4 cemented fragments of earlier anhydrite grains including Anh1 and Anh2.

The second generation (Anh2) shows bright to grey CL with "wavy" oscillatory boundaries (Figure 7a,b), with Anh2a being brighter and Anh2b darker.

The third generation of anhydrite (Anh3) occurred as euhedral crystals overgrowing Anh1 or infilled interstitial spaces of Anh1 and Anh2 (Figure 7a,c). They are subdivided to Anh3a and Anh3b according to CL intensity and zoning patterns (Figure 7c). Anh3a is brighter in CL and shows evident oscillatory zoning in contrast to Anh3b.

The last generation of anhydrite (Anh4) is anhedral and CL-dark (Figure 7d). Anh4 may cement Anh1 and Anh2 fragments (Figure 7e). All anhydrite generations except Anh3 have been found in both A.Vaq and B.Vmacpq.

Mineralogical and textural interpretations suggest a sequential co-precipitation of Qz1 and hematite, Qz2a and Anh1a, Qz2b and Anh1b, Qz3 and Anh2, along with pyrite and rutile, Qz4, and Anh4 along with chalcopyrite, pyrite, rutile, molybdenite, and Qz5 along with pyrite, apatite, rutile, and gypsum (Table 2).
D.Vpd veins, and are intimately associated with pyrite. Locally, they occur as dark bands crosscutting or filling the interstitial space of earlier quartz (Figure 6j).

The latest generation of quartz (Qz6) comprises a CL-dark to grey interior (Qz6a) and a very bright-CL exterior (Qz6b) (Figure 6k). They were observed in the A.Vaq, D.Vpq, and D.Vpd. Qz6a exhibited an oscillation of red and blue CL, whereas Qz6b displayed a bright yellowish blue (Figure 6l).

Four generations of anhydrite have been identified. The first generation of anhydrite (Anh1) exhibited bright, homogeneous to patchy CL (Figure 7a). They are subdivided to Anh1a and Anh1b according to CL intensity. Anh1a grains have higher CL intensity and irregular boundaries (Figure 7a) relative to Anh1b grains that are commonly overgrown, recrystallized, or crosscut by later anhydrites.

<figure><img src="image_9.png" /></figure>

**Figure 7.** Cathodoluminescence (CL) micro textures of vein anhydrite at the Tongchang porphyry Cu deposit. (a) The first generation of anhydrite (Anh1), rimed and surrounded by CL-oscillatory Anh2, coexisting with pyrite and quartz; (b) Anh2a showing “wavy” oscillatory zoning; (c) A cluster of euhedral Anh3a and Anh3b grains, with Anh3a showing oscillatory zoning, whereas Anh3b showed homogeneous CL; (d,e) CL-dark Anh4 cemented fragments of earlier anhydrite grains including Anh1 and Anh2.

The second generation (Anh2) shows bright to grey CL with “wavy” oscillatory boundaries (Figure 7a,b), with Anh2a being brighter and Anh2b darker.

The third generation of anhydrite (Anh3) occurred as euhedral crystals overgrowing Anh1 or infilled interstitial spaces of Anh1 and Anh2 (Figure 7a,c). They are subdivided to Anh3a and Anh3b according to CL intensity and zoning patterns (Figure 7c). Anh3a is brighter in CL and shows evident oscillatory zoning in contrast to Anh3b.

The last generation of anhydrite (Anh4) is anhedral and CL-dark (Figure 7d). Anh4 may cement Anh1 and Anh2 fragments (Figure 7e). All anhydrite generations except Anh3 have been found in both A.Vaq and B.Vmacpq.

Mineralogical and textural interpretations suggest a sequential co-precipitation of Qz1 and hematite, Qz2a and Anh1a, Qz2b and Anh1b, Qz3 and Anh2, along with pyrite and rutile, Qz4, and Anh4 along with chalcopyrite, pyrite, rutile, molybdenite, and Qz5 along with pyrite, apatite, rutile, and gypsum (Table 2).
<table><caption>**Table 2.** A summary of generations, CL textures, mineral assemblages and Ti contents of quartz and anhydrite of the Tongchang porphyry Cu deposit.</caption><thead><tr><th>Qz</th><th>Anh</th><th>Other Vein Minerals</th><th>CL</th><th>Ti (ppm)</th><th>Occurrence in Sample</th></tr></thead><tbody><tr><td>Qz1</td><td></td><td>hematite</td><td>Qz: granular, homogeneous to faint zoning, grey.</td><td>27-43</td><td>10DX261, 12LDX37, 12LDX40</td></tr><tr><td>Qz2a</td><td>Anh1a</td><td>K-feldspar, hematite, magnetite</td><td>Qz: subhedral, oscillatory zoning, bright.<br>Anh: homogeneous, bright.</td><td>80-220</td><td>10DX22, 10DX172, 10DX328,<br>12DXF05, 12DX500</td></tr><tr><td>Qz2b</td><td>Anh1b</td><td>hematite, magnetite</td><td>Qz: homogeneous to oscillatory zoning, bright.<br>Anh: homogeneous, bright</td><td>50-70</td><td>10DX22, 10DX140, 10DX168,<br>10DX172, 10DX197, 10DX328,<br>12DXF05, 12DX500</td></tr><tr><td>Qz3a</td><td>Anh2a</td><td>rutile, hematite, magnetite</td><td>Qz: homogeneous, dark.<br>Anh: euhedral oscillatory zoning</td><td>7-16</td><td>10DX140, 10DX168, 10DX197,<br>10DX220, 10DX261, 10DX328</td></tr><tr><td>Qz3b</td><td>Anh2b</td><td>epidote, rutile, pyrite, hematite,<br>magnetite</td><td>Qz: euhedral oscillatory zoning.<br>Anh: euhedral oscillatory zoning</td><td>2-35</td><td></td></tr><tr><td>Qz4</td><td>Anh4</td><td>chlorite, sericite, rutile, bornite,<br>chalcopyrite, pyrite, magnetite,<br>monazite, apatite, epidote</td><td>Qz: homogeneous, dark.<br>Anh: subhedral to euhedral homogeneous, dark.</td><td>3-17</td><td>10DX168, 10DX261, 10DX328,<br>12LDX37</td></tr><tr><td>Qz5a</td><td></td><td>sericite, muscovite, pyrite,</td><td>Qz: homogeneous, dark.</td><td>8-10</td><td>10DX164</td></tr><tr><td>Qz5b</td><td></td><td>molybdenite, rutile, apatite, gypsum</td><td>Qz: euhedral oscillatory zoning.</td><td>1-15</td><td>10DX140, 10DX145, 10DX164,<br>10DX201, 10DX220</td></tr><tr><td>Qz6a</td><td></td><td>Not observed</td><td>Qz: euhedral oscillatory zoning, dark to grey.</td><td>3-8</td><td></td></tr><tr><td>Qz6b</td><td></td><td>Not observed</td><td>Qz: euhedral oscillatory zoning, very bright.</td><td>0.3-2</td><td>10DX140, 10DX158, 10DX201</td></tr></tbody></table>
<table><caption>**Table 2.** A summary of generations, CL textures, mineral assemblages and Ti contents of quartz and anhydrite of the Tongchang porphyry Cu deposit.</caption><thead><tr><th>Qz</th><th>Anh</th><th>Other Vein Minerals</th><th>CL</th><th>Ti (ppm)</th><th>Occurrence in Sample</th></tr></thead><tbody><tr><td>Qz1</td><td></td><td>hematite</td><td>Qz: granular, homogeneous to faint zoning, grey.</td><td>27-43</td><td>10DX261, 12LDX37, 12LDX40</td></tr><tr><td>Qz2a</td><td>Anh1a</td><td>K-feldspar, hematite, magnetite</td><td>Qz: subhedral, oscillatory zoning, bright.<br>Anh: homogeneous, bright.</td><td>80-220</td><td>10DX22, 10DX172, 10DX328,<br>12DXF05, 12DX500</td></tr><tr><td>Qz2b</td><td>Anh1b</td><td>hematite, magnetite</td><td>Qz: homogeneous to oscillatory zoning, bright.<br>Anh: homogeneous, bright</td><td>50-70</td><td>10DX22, 10DX140, 10DX168,<br>10DX172, 10DX197, 10DX328,<br>12DXF05, 12DX500</td></tr><tr><td>Qz3a</td><td>Anh2a</td><td>rutile, hematite, magnetite</td><td>Qz: homogeneous, dark.<br>Anh: euhedral oscillatory zoning</td><td>7-16</td><td>10DX140, 10DX168, 10DX197,<br>10DX220, 10DX261, 10DX328</td></tr><tr><td>Qz3b</td><td>Anh2b</td><td>epidote, rutile, pyrite, hematite,<br>magnetite</td><td>Qz: euhedral oscillatory zoning.<br>Anh: euhedral oscillatory zoning</td><td>2-35</td><td></td></tr><tr><td>Qz4</td><td>Anh4</td><td>chlorite, sericite, rutile, bornite,<br>chalcopyrite, pyrite, magnetite,<br>monazite, apatite, epidote</td><td>Qz: homogeneous, dark.<br>Anh: subhedral to euhedral homogeneous, dark.</td><td>3-17</td><td>10DX168, 10DX261, 10DX328,<br>12LDX37</td></tr><tr><td>Qz5a</td><td></td><td>sericite, muscovite, pyrite,</td><td>Qz: homogeneous, dark.</td><td>8-10</td><td>10DX164</td></tr><tr><td>Qz5b</td><td></td><td>molybdenite, rutile, apatite, gypsum</td><td>Qz: euhedral oscillatory zoning.</td><td>1-15</td><td>10DX140, 10DX145, 10DX164,<br>10DX201, 10DX220</td></tr><tr><td>Qz6a</td><td></td><td>Not observed</td><td>Qz: euhedral oscillatory zoning, dark to grey.</td><td>3-8</td><td></td></tr><tr><td>Qz6b</td><td></td><td>Not observed</td><td>Qz: euhedral oscillatory zoning, very bright.</td><td>0.3-2</td><td>10DX140, 10DX158, 10DX201</td></tr></tbody></table>
## 5.2. Fluid Inclusions

Fluid inclusions at Tongchang were named using the nomenclature of [74] based on the relative volume fraction of bubbles and solid species (e.g., B15HS denotes 15% vapor phase, a halite daughter, and an opaque solid). Fluid inclusion assemblages (FIA) and their origin were determined with the aid of CL micro textures. Microthermometric temperatures and estimated salinity, density, and pressure are listed in Table 3.

<table><caption>**Table 3.** Fluid inclusion microthermometry of the Tongchang porphyry Cu deposit.</caption><thead><tr><th>Type</th><th>Host Qz</th><th>T<sub>m,ice</sub><br>(°C)</th><th>T<sub>m,halite</sub><br>(°C)</th><th>Thv (°C)</th><th>Salinity<br>(wt.%)</th><th>Density<br>(g/cm<sup>3</sup>)</th><th>dP/dT<br>(bar/°C)</th><th>Homo.<br>Mode</th></tr></thead><tbody><tr><td rowspan="4">B15HS</td><td>primary in<br>QZ2a in<br>12DX500</td><td>\</td><td>458.4</td><td>369.7</td><td>54.2</td><td>1.2</td><td>19.1</td><td rowspan="4">halite<br>dissolution</td></tr><tr><td></td><td>\</td><td>469.2</td><td>382.8</td><td>55.4</td><td>1.2</td><td>18.7</td></tr><tr><td></td><td>\</td><td>512.1</td><td>415.3</td><td>60.4</td><td>1.2</td><td>20.3</td></tr><tr><td>primary in<br>Qz2b in<br>10DX168</td><td>-1.1</td><td>387.9</td><td>279.7</td><td>46.7</td><td>1.2</td><td>23.7</td></tr><tr><td rowspan="12">B80</td><td></td><td>\</td><td>396.1</td><td>269.4</td><td>47.4</td><td>1.2</td><td>26.2</td><td rowspan="12">critical</td></tr><tr><td></td><td>\</td><td>403.5</td><td>403.5</td><td>\</td><td>\</td><td>\</td></tr><tr><td></td><td>-4.2</td><td>344.6</td><td>344.6</td><td>6.7</td><td>0.7</td><td>8.5</td></tr><tr><td></td><td>\</td><td>356.8</td><td>356.8</td><td>\</td><td>\</td><td>\</td></tr><tr><td></td><td>\</td><td>316.5</td><td>316.5</td><td>\</td><td>\</td><td>\</td></tr><tr><td rowspan="8">B50</td><td>primary in<br>Qz3b in<br>10DX168</td><td>\</td><td>320.7</td><td>320.7</td><td>\</td><td>\</td><td>\</td></tr><tr><td></td><td>\</td><td>300.6</td><td>300.6</td><td>\</td><td>\</td><td>\</td></tr><tr><td></td><td>\</td><td>359.4</td><td>359.4</td><td>\</td><td>\</td><td>\</td></tr><tr><td></td><td>-3.6</td><td>343.4</td><td>343.4</td><td>5.9</td><td>0.7</td><td>8.3</td></tr><tr><td></td><td>-2.7</td><td>299.6</td><td>299.6</td><td>4.5</td><td>0.8</td><td>10.4</td></tr><tr><td></td><td>-5.6</td><td>284.5</td><td>284.5</td><td>8.7</td><td>0.8</td><td>11.9</td></tr><tr><td></td><td>-3.2</td><td>287.5</td><td>287.5</td><td>5.3</td><td>0.8</td><td>11.2</td></tr><tr><td></td><td>-3.3</td><td>275.6</td><td>275.6</td><td>5.4</td><td>0.8</td><td>11.9</td></tr><tr><td rowspan="8">B30</td><td>secondary<br>in Qz2b<br>and Qz3b<br>primary in<br>10DX168</td><td>\</td><td>272.6</td><td>272.6</td><td>\</td><td>\</td><td>\</td></tr><tr><td></td><td>\</td><td>255.5</td><td>255.5</td><td>\</td><td>\</td><td>\</td></tr><tr><td></td><td>\</td><td>226.2</td><td>226.2</td><td>\</td><td>\</td><td>\</td></tr><tr><td></td><td>\</td><td>262</td><td>262</td><td>\</td><td>\</td><td>\</td></tr><tr><td></td><td>-4.8</td><td>248.9</td><td>248.9</td><td>7.6</td><td>0.9</td><td>13.6</td></tr><tr><td></td><td>\</td><td>257.5</td><td>257.5</td><td>\</td><td>\</td><td>\</td></tr><tr><td></td><td>\</td><td>278.3</td><td>278.3</td><td>\</td><td>\</td><td>\</td></tr><tr><td></td><td>\</td><td>248.9</td><td>248.9</td><td>\</td><td>\</td><td>\</td></tr><tr><td rowspan="6">B10</td><td rowspan="6">secondary<br>in Qz2b in<br>10DX168</td><td>\</td><td>198.5</td><td>198.5</td><td>\</td><td>\</td><td>\</td></tr><tr><td>\</td><td>212.3</td><td>212.3</td><td>\</td><td>\</td><td>\</td></tr><tr><td>\</td><td>213.7</td><td>213.7</td><td>\</td><td>\</td><td>\</td></tr><tr><td>\</td><td>210.8</td><td>210.8</td><td>\</td><td>\</td><td>\</td></tr><tr><td>-2.6</td><td>207.9</td><td>207.9</td><td>4.3</td><td>0.9</td><td>15.3</td></tr><tr><td>-3.4</td><td>186.6</td><td>186.6</td><td>5.6</td><td>0.9</td><td>16.6</td></tr></tbody></table>

Due to intense recrystallization, Qz1 grains are devoid of primary FIAs, but flooded with secondary FIAs in healed fractures. Qz2a and Qz2b quartz host primary FIAs of B15HS and B80 inclusions (Figure 8a,b). B15HS inclusions in Qz2a and Qz2b showed different temperatures of halite dissolution and vapor disappearance. In Qz2a grains, B15HS showed halite dissolution at 458–512 °C and vapor disappearance at 370–415 °C, whereas those in Qz2b grains showed lower halite-dissolution temperatures (388–396 °C) and vapor disappearance temperatures (270–280 °C). One B80 inclusion in Qz2b was homogenized at 404 °C via critical mode.
## 5.2. Fluid Inclusions

Fluid inclusions at Tongchang were named using the nomenclature of [74] based on the relative volume fraction of bubbles and solid species (e.g., B15HS denotes 15% vapor phase, a halite daughter, and an opaque solid). Fluid inclusion assemblages (FIA) and their origin were determined with the aid of CL micro textures. Microthermometric temperatures and estimated salinity, density, and pressure are listed in Table 3.

<table><caption>**Table 3.** Fluid inclusion microthermometry of the Tongchang porphyry Cu deposit.</caption><thead><tr><th>Type</th><th>Host Qz</th><th>T<sub>m,ice</sub><br>(°C)</th><th>T<sub>m,halite</sub><br>(°C)</th><th>Thv (°C)</th><th>Salinity<br>(wt.%)</th><th>Density<br>(g/cm³)</th><th>dP/dT<br>(bar/°C)</th><th>Homo.<br>Mode</th></tr></thead><tbody><tr><td rowspan="4">B15HS</td><td>primary in<br>QZ2a in<br>12DX500</td><td>\</td><td>458.4</td><td>369.7</td><td>54.2</td><td>1.2</td><td>19.1</td><td rowspan="4">halite<br>dissolution</td></tr><tr><td>\</td><td>469.2</td><td>382.8</td><td>55.4</td><td>1.2</td><td>18.7</td></tr><tr><td>\</td><td>512.1</td><td>415.3</td><td>60.4</td><td>1.2</td><td>20.3</td></tr><tr><td>primary in<br>Qz2b in<br>10DX168</td><td>-1.1</td><td>387.9</td><td>279.7</td><td>46.7</td><td>1.2</td><td>23.7</td></tr><tr><td rowspan="12">B80</td><td>\</td><td>396.1</td><td>269.4</td><td>47.4</td><td>1.2</td><td>26.2</td><td rowspan="12">critical</td></tr><tr><td>\</td><td>403.5</td><td>403.5</td><td>\</td><td>\</td><td>\</td></tr><tr><td>-4.2</td><td>344.6</td><td>344.6</td><td>6.7</td><td>0.7</td><td>8.5</td></tr><tr><td>\</td><td>356.8</td><td>356.8</td><td>\</td><td>\</td><td>\</td></tr><tr><td>\</td><td>316.5</td><td>316.5</td><td>\</td><td>\</td><td>\</td></tr><tr><td>\</td><td>320.7</td><td>320.7</td><td>\</td><td>\</td><td>\</td></tr><tr><td>\</td><td>300.6</td><td>300.6</td><td>\</td><td>\</td><td>\</td></tr><tr><td>\</td><td>359.4</td><td>359.4</td><td>\</td><td>\</td><td>\</td></tr><tr><td>-3.6</td><td>343.4</td><td>343.4</td><td>5.9</td><td>0.7</td><td>8.3</td></tr><tr><td>-2.7</td><td>299.6</td><td>299.6</td><td>4.5</td><td>0.8</td><td>10.4</td></tr><tr><td rowspan="12">B50</td><td>\</td><td>284.5</td><td>284.5</td><td>8.7</td><td>0.8</td><td>11.9</td><td rowspan="12">to liquid</td></tr><tr><td>-5.6</td><td>284.5</td><td>284.5</td><td>8.7</td><td>0.8</td><td>11.9</td></tr><tr><td>-3.2</td><td>287.5</td><td>287.5</td><td>5.3</td><td>0.8</td><td>11.2</td></tr><tr><td>-3.3</td><td>275.6</td><td>275.6</td><td>5.4</td><td>0.8</td><td>11.9</td></tr><tr><td>\</td><td>272.6</td><td>272.6</td><td>\</td><td>\</td><td>\</td></tr><tr><td>\</td><td>255.5</td><td>255.5</td><td>\</td><td>\</td><td>\</td></tr><tr><td>\</td><td>226.2</td><td>226.2</td><td>\</td><td>\</td><td>\</td></tr><tr><td>\</td><td>262</td><td>262</td><td>\</td><td>\</td><td>\</td></tr><tr><td>-4.8</td><td>248.9</td><td>248.9</td><td>7.6</td><td>0.9</td><td>13.6</td></tr><tr><td>\</td><td>257.5</td><td>257.5</td><td>\</td><td>\</td><td>\</td></tr><tr><td>\</td><td>278.3</td><td>278.3</td><td>\</td><td>\</td><td>\</td></tr><tr><td>\</td><td>248.9</td><td>248.9</td><td>\</td><td>\</td><td>\</td></tr><tr><td rowspan="12">B30</td><td>\</td><td>198.5</td><td>198.5</td><td>\</td><td>\</td><td>\</td><td rowspan="12">to liquid</td></tr><tr><td>\</td><td>212.3</td><td>212.3</td><td>\</td><td>\</td><td>\</td></tr><tr><td>\</td><td>213.7</td><td>213.7</td><td>\</td><td>\</td><td>\</td></tr><tr><td>\</td><td>210.8</td><td>210.8</td><td>\</td><td>\</td><td>\</td></tr><tr><td>-2.6</td><td>207.9</td><td>207.9</td><td>4.3</td><td>0.9</td><td>15.3</td></tr><tr><td>-3.4</td><td>186.6</td><td>186.6</td><td>5.6</td><td>0.9</td><td>16.6</td></tr></tbody></table>

Due to intense recrystallization, Qz1 grains are devoid of primary FIAs, but flooded with secondary FIAs in healed fractures. Qz2a and Qz2b quartz host primary FIAs of B15HS and B80 inclusions (Figure 8a,b). B15HS inclusions in Qz2a and Qz2b showed different temperatures of halite dissolution and vapor disappearance. In Qz2a grains, B15HS showed halite dissolution at 458–512 °C and vapor disappearance at 370–415 °C, whereas those in Qz2b grains showed lower halite-dissolution temperatures (388–396 °C) and vapor disappearance temperatures (270–280 °C). One B80 inclusion in Qz2b was homogenized at 404 °C via critical mode.
<figure><img src="image_10.png" /></figure>

**Figure 8.** Petrography of fluid inclusions hosted in different generations of quartz in the Tongchang porphyry Cu deposit. The coexistence of brine (B15HS) and vapor-rich (B80) inclusions in Qz2a (a) and Qz2b (b), which distributed along CL growth zones indicative of primary origin; primary B50 inclusions in Qz3b with secondary trails of B80 and B30 inclusions (c); secondary trail of B10 inclusion in Qz2b (d). "B10" denotes the vapor phase and its volume proportion relative to the total inclusion volume; "L" denotes aqueous liquid, "V" denotes vapor, "H" denotes a halite daughter phase, and "S" denotes unidentified solids. CL growth zones are marked with dashed curves in the inclusion images. Scale bars are 10 µm.

Qz3b contains primary B50 inclusions (Figure 8c). They had ice melting temperatures of -2.7-4.2 °C and were homogenized at 300-350 °C via critical mode or vapor expansion.

Qz4 commonly contains only B30 inclusions, which are considered primary. They exhibited ice melting at -3.2-5.6 °C and were homogenized at 250-300 °C. They also occurred as secondary inclusions in Qz2 and Qz3 (Figure 8c). B10 occurred mainly as secondary inclusions in Qz2 and Qz3. It had ice melting temperatures at -2.6-3.4 °C and was homogenized at 187-208 °C.

### 5.3. Trace Elements

Results are shown and depicted in Figure 9, Table 4, and the Appendix A. In all quartz generations, only Ti, Li, Na, Al, K, and Ge occurred in appreciable concentrations. Arsenic and Sb becomes significant in Qz5 and Qz6.

<figure><img src="image_11.png" /></figure>
<figure><img src="image_10.png" /></figure>

**Figure 8.** Petrography of fluid inclusions hosted in different generations of quartz in the Tongchang porphyry Cu deposit. The coexistence of brine (B15HS) and vapor-rich (B80) inclusions in Qz2a (a) and Qz2b (b), which distributed along CL growth zones indicative of primary origin; primary B50 inclusions in Qz3b with secondary trails of B80 and B30 inclusions (c); secondary trail of B10 inclusion in Qz2b (d). "B10" denotes the vapor phase and its volume proportion relative to the total inclusion volume; "L" denotes aqueous liquid, "V" denotes vapor, "H" denotes a halite daughter phase, and "S" denotes unidentified solids. CL growth zones are marked with dashed curves in the inclusion images. Scale bars are 10 µm.

Qz3b contains primary B50 inclusions (Figure 8c). They had ice melting temperatures of -2.7-4.2 °C and were homogenized at 300-350 °C via critical mode or vapor expansion.

Qz4 commonly contains only B30 inclusions, which are considered primary. They exhibited ice melting at -3.2-5.6 °C and were homogenized at 250-300 °C. They also occurred as secondary inclusions in Qz2 and Qz3 (Figure 8c). B10 occurred mainly as secondary inclusions in Qz2 and Qz3. It had ice melting temperatures at -2.6-3.4 °C and was homogenized at 187-208 °C.

### 5.3. Trace Elements

Results are shown and depicted in Figure 9, Table 4, and the Appendix A. In all quartz generations, only Ti, Li, Na, Al, K, and Ge occurred in appreciable concentrations. Arsenic and Sb becomes significant in Qz5 and Qz6.

<figure><img src="image_11.png" /></figure>
<figure><img src="image_12.png" /></figure>

<figure><img src="image_13.png" /></figure>
<figure><img src="image_12.png" /></figure>

<figure><img src="image_13.png" /></figure>
<figure><img src="image_14.png" /></figure>

**Figure 9.** Sketches showing quartz CL textures and ablation spots for trace elements. (a) B.V<sub>cpq</sub> vein crosscutting the A.V<sub>qd</sub> vein (12LDX37). Qz1 had intermediate Ti contents (20–30 ppm); Qz2 had higher Ti contents (50–70 ppm). Note that Cu-Fe sulfides coprecipitated with Qz4, which reopened Qz2 grains. Qz2 grains, in turn, crosscut Qz1 grains; (b) In D.V<sub>pd</sub> pyrite veins (10DX140), Qz3 had lower Ti contents (10–20 ppm) compared to earlier quartz; (c) A profile of trace element analyses encompassing Qz3, Qz5, and Qz6 (10DX201). Qz5 had variable yet lower Ti contents (1–15 ppm). Qz6a and Qz6b had elevated contents of Ge, As and Sb.

Titanium contents show characteristic patterns among quartz generations. It increases from 26.8 ± 10.3 ppm (1σ, N = 59) in Qz1 to 127 ± 37 ppm (1σ, N = 42) in Qz2a and then decreases to 53.9 ± 16.1 ppm (1σ, N = 163) in Qz2b, 10.7 ± 4.0 ppm (1σ, N = 21) in Qz3a, 15 ± 7.9 ppm (1σ, N = 131) in Qz3b, 6.74 ± 4.22 ppm (1σ, N = 24) in Qz4, 8.40 ± 0.88 ppm (1σ, N = 4) in Qz5a, 7.66 ± 4.06 ppm (1σ, N = 66) in Qz5b, 2.67 ± 2.19 ppm (1σ, N = 19) in Qz6a, and 0.699 ± 0.454 ppm in Qz6b.

Lithium increases slightly from 11 ppm in Qz1 to av. 19 ppm in Qz3b, then decreases to 8 ppm in Qz4, and increases to 70 ppm in Qz6a which decreases to 29 ppm in Qz6b. Al increases from 172 ppm in Qz1 to 578 ppm in Qz3b, and then decreases to 300 ppm in Qz4, and then increases to 923 ppm in Qz6a which decreases to 718 ppm in Qz6b. Ge increases from 1 ppm in Qz1 to 14 ppm in Qz6b. As increases from 1 ppm in early quartz to 31 ppm in Qz6b, and Sb increases from 0 ppm (below detection limits) in early quartz to 20 ppm in Qz6a and 207 ppm in Qz6b.
<figure><img src="image_14.png" /></figure>

**Figure 9.** Sketches showing quartz CL textures and ablation spots for trace elements. (a) B.V<sub>cpq</sub> vein crosscutting the A.V<sub>qd</sub> vein (12LDX37). Qz1 had intermediate Ti contents (20–30 ppm); Qz2 had higher Ti contents (50–70 ppm). Note that Cu-Fe sulfides coprecipitated with Qz4, which reopened Qz2 grains. Qz2 grains, in turn, crosscut Qz1 grains; (b) In D.V<sub>pd</sub> pyrite veins (10DX140), Qz3 had lower Ti contents (10–20 ppm) compared to earlier quartz; (c) A profile of trace element analyses encompassing Qz3, Qz5, and Qz6 (10DX201). Qz5 had variable yet lower Ti contents (1–15 ppm). Qz6a and Qz6b had elevated contents of Ge, As and Sb.

Titanium contents show characteristic patterns among quartz generations. It increases from 26.8 ± 10.3 ppm (1σ, N = 59) in Qz1 to 127 ± 37 ppm (1σ, N = 42) in Qz2a and then decreases to 53.9 ± 16.1 ppm (1σ, N = 163) in Qz2b, 10.7 ± 4.0 ppm (1σ, N = 21) in Qz3a, 15 ± 7.9 ppm (1σ, N = 131) in Qz3b, 6.74 ± 4.22 ppm (1σ, N = 24) in Qz4, 8.40 ± 0.88 ppm (1σ, N = 4) in Qz5a, 7.66 ± 4.06 ppm (1σ, N = 66) in Qz5b, 2.67 ± 2.19 ppm (1σ, N = 19) in Qz6a, and 0.699 ± 0.454 ppm in Qz6b.

Lithium increases slightly from 11 ppm in Qz1 to av. 19 ppm in Qz3b, then decreases to 8 ppm in Qz4, and increases to 70 ppm in Qz6a which decreases to 29 ppm in Qz6b. Al increases from 172 ppm in Qz1 to 578 ppm in Qz3b, and then decreases to 300 ppm in Qz4, and then increases to 923 ppm in Qz6a which decreases to 718 ppm in Qz6b. Ge increases from 1 ppm in Qz1 to 14 ppm in Qz6b. As increases from 1 ppm in early quartz to 31 ppm in Qz6b, and Sb increases from 0 ppm (below detection limits) in early quartz to 20 ppm in Qz6a and 207 ppm in Qz6b.
<table><caption>Table 4. LA-ICP-MS trace elements in quartz of the Tongchang porphyry Cu deposit.</caption><thead><tr><th>Spot No.</th><th>CL</th><th>Li</th><th>Na</th><th>Al</th><th>K</th><th>Ca</th><th>Ti</th><th>Mn</th><th>Fe</th><th>Cu</th><th>Zn</th><th>Ga</th><th>Ge</th><th>As</th><th>Sr</th><th>Sn</th><th>Sb</th><th>Pb</th><th>Al Factor</th><th>Al Corr</th><th>P min (kbar)</th><th>P max (kbar)</th><th>Tmin (°C)</th><th>Tmax (°C)</th></tr></thead><tbody><tr><td>12LDX37-1</td><td>Qz1</td><td>9.26</td><td>54.6</td><td>290</td><td>229</td><td>&lt;86.01</td><td>43.2</td><td>1.72</td><td>v.d.</td><td>1.00</td><td>0.78</td><td>0.205</td><td>1.10</td><td>0.490</td><td>1.03</td><td>0.13</td><td>1.59</td><td>1.35</td><td>0.7</td><td>414</td><td>0.5</td><td>1.5</td><td>461</td><td>538</td></tr><tr><td>12LDX37-2</td><td>Qz1</td><td>11.2</td><td>187</td><td>74.3</td><td>49.2</td><td>&lt;39.88</td><td>38.0</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.0207</td><td>1.28</td><td>0.304</td><td>0.31</td><td>0.119</td><td>0.792</td><td>v.d.</td><td>0.7</td><td>106</td><td>0.5</td><td>1.5</td><td>453</td><td>528</td></tr><tr><td>12LDX37-7</td><td>Qz1</td><td>10.6</td><td>v.d.</td><td>65.5</td><td>v.d.</td><td>v.d.</td><td>43.4</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>1.36</td><td>v.d.</td><td>v.d.</td><td>0.100</td><td>0.773</td><td>v.d.</td><td>0.7</td><td>93.6</td><td>0.5</td><td>1.5</td><td>462</td><td>538</td></tr><tr><td>12LDX37-8</td><td>Qz1</td><td>10.0</td><td>120</td><td>134</td><td>104</td><td>&lt;88.69</td><td>35.0</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.0440</td><td>0.83<br>1</td><td>0.350</td><td>0.39</td><td>&lt;0.06<br>2</td><td>0.587</td><td>2.57</td><td>0.7</td><td>191</td><td>0.5</td><td>1.5</td><td>448</td><td>522</td></tr><tr><td>12LDX37-9</td><td>Qz1</td><td>10.8</td><td>689</td><td>74.3</td><td>v.d.</td><td>v.d.</td><td>29.7</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.399</td><td>v.d.</td><td>0.142</td><td>0.467</td><td>v.d.</td><td>0.7</td><td>106</td><td>0.5</td><td>1.5</td><td>438</td><td>510</td></tr><tr><td>12LDX37-14</td><td>Qz1</td><td>6.59</td><td>v.d.</td><td>118</td><td>56.9</td><td>240</td><td>30.5</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.0270</td><td>0.87<br>0</td><td>&lt;0.43</td><td>1.16</td><td>0.207</td><td>v.d.</td><td>v.d.</td><td>0.7</td><td>168</td><td>0.5</td><td>1.5</td><td>439</td><td>512</td></tr><tr><td>12LDX37-15</td><td>Qz1</td><td>7.32</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>109</td><td>35.9</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.0310</td><td>1.1</td><td>0.670</td><td>v.d.</td><td>0.098</td><td>0.561</td><td>v.d.</td><td>0.7</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>450</td><td>524</td></tr><tr><td>12LDX37-36</td><td>Qz1</td><td>13.5</td><td>18.1</td><td>176<br>2</td><td>599</td><td>445</td><td>36.7</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>&lt;1.01</td><td>0.346</td><td>1.41</td><td>0.420</td><td>2.56</td><td>0.054<br>0</td><td>0.378</td><td>0.116</td><td>0.7</td><td>2518</td><td>0.5</td><td>1.5</td><td>451</td><td>525</td></tr><tr><td>12LDX37-34</td><td>Qz1</td><td>7.30</td><td>&lt;2.7<br>1</td><td>135</td><td>28.17</td><td>234</td><td>28.8</td><td>0.711</td><td>v.d.</td><td>1.01</td><td>&lt;0.94</td><td>0.223</td><td>1.31</td><td>0.680</td><td>0.171</td><td>&lt;0.07<br>9</td><td>&lt;0.08<br>0</td><td>0.227</td><td>0.7</td><td>192</td><td>0.5</td><td>1.5</td><td>436</td><td>507</td></tr><tr><td>12LDX37-40</td><td>Qz1</td><td>10.3</td><td>&lt;3.7<br>8</td><td>87.1</td><td>&lt;6.91</td><td>&lt;140.4<br>5</td><td>43.9</td><td>0.144</td><td>2.26</td><td>0.730</td><td>1.65</td><td>0.107</td><td>0.86<br>0</td><td>0.580</td><td>0.221</td><td>&lt;0.08<br>8</td><td>&lt;0.06<br>7</td><td>0.09</td><td>0.7</td><td>124</td><td>0.5</td><td>1.5</td><td>463</td><td>539</td></tr><tr><td>12LDX37-42</td><td>Qz1</td><td>10.2</td><td>141</td><td>70.6</td><td>60.8</td><td>v.d.</td><td>32.3</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.216</td><td>1.58</td><td>0.360</td><td>v.d.</td><td>0.240</td><td>0.199</td><td>1.85</td><td>0.7</td><td>101</td><td>0.5</td><td>1.5</td><td>443</td><td>516</td></tr><tr><td>12LDX37-43</td><td>Qz1</td><td>7.84</td><td>18.9</td><td>58.8</td><td>5.13</td><td>&lt;88.42</td><td>23.2</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.950</td><td>0.247</td><td>1.13</td><td>&lt;0.33</td><td>0.587</td><td>&lt;0.08<br>3</td><td>0.317</td><td>1.02</td><td>0.7</td><td>84.0</td><td>0.5</td><td>1.5</td><td>422</td><td>492</td></tr><tr><td>12LDX37-44</td><td>Qz1</td><td>10.5</td><td>v.d.</td><td>61.3</td><td>v.d.</td><td>457</td><td>24.5</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.079</td><td>1.06</td><td>0.270</td><td>v.d.</td><td>0.162</td><td>0.098</td><td>v.d.</td><td>0.7</td><td>87.6</td><td>0.5</td><td>1.5</td><td>426</td><td>496</td></tr><tr><td>12LDX37-45</td><td>Qz1</td><td>11.3</td><td>&lt;2.9<br>0</td><td>88.8</td><td>&lt;5.24</td><td>&lt;103.2<br>6</td><td>24.9</td><td>0.143</td><td>4.14</td><td>&lt;0.31</td><td>1.50</td><td>0.143</td><td>0.84<br>0</td><td>&lt;0.28<br>8</td><td>0.054</td><td>&lt;0.08<br>1</td><td>&lt;0.08<br>0</td><td>0.096</td><td>0.7</td><td>127</td><td>0.5</td><td>1.5</td><td>427</td><td>497</td></tr><tr><td>12LDX37-46</td><td>Qz1</td><td>10.8</td><td>6.73</td><td>71.6</td><td>8.02</td><td>&lt;58.04</td><td>32.8</td><td>0.819</td><td>v.d.</td><td>0.418</td><td>&lt;0.67</td><td>&lt;0.013<br>3</td><td>0.97<br>5</td><td>0.239</td><td>1.05</td><td>0.055</td><td>&lt;0.04<br>2</td><td>0.233</td><td>0.7</td><td>102</td><td>0.5</td><td>1.5</td><td>444</td><td>517</td></tr><tr><td>12LDX37-47</td><td>Qz1</td><td>10.3</td><td>8.08</td><td>76.1</td><td>&lt;4.52</td><td>99.3</td><td>24.0</td><td>0.237</td><td>4.18</td><td>0.290</td><td>&lt;0.53</td><td>0.130</td><td>1.19</td><td>&lt;0.33</td><td>0.773</td><td>0.190</td><td>0.206</td><td>0.103</td><td>0.7</td><td>109</td><td>0.5</td><td>1.5</td><td>424</td><td>494</td></tr><tr><td>12LDX37-48</td><td>Qz1</td><td>11.2</td><td>v.d.</td><td>64.4</td><td>69.6</td><td>v.d.</td><td>23.4</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.0620</td><td>0.85<br>0</td><td>&lt;0.35</td><td>v.d.</td><td>0.179</td><td>0.113</td><td>v.d.</td><td>0.7</td><td>91.9</td><td>0.5</td><td>1.5</td><td>423</td><td>492</td></tr><tr><td>12LDX37-49</td><td>Qz1</td><td>10.3</td><td>18.8</td><td>99.5</td><td>&lt;5.31</td><td>591</td><td>36.6</td><td>0.105</td><td>2.38</td><td>&lt;0.34</td><td>1.63</td><td>0.348</td><td>1.50</td><td>0.730</td><td>1.29</td><td>0.095</td><td>0.679</td><td>0.259</td><td>0.7</td><td>142</td><td>0.5</td><td>1.5</td><td>451</td><td>525</td></tr><tr><td>12LDX37-50</td><td>Qz1</td><td>12.6</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>30.5</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.134</td><td>1.20</td><td>1.59</td><td>v.d.</td><td>0.177</td><td>1.68</td><td>v.d.</td><td>0.7</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>439</td><td>512</td></tr><tr><td>12LDX40-1</td><td>Qz1</td><td>12.0</td><td>83.0</td><td>67.6</td><td>28.2</td><td>614</td><td>37.8</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.112</td><td>1.64</td><td>0.640</td><td>v.d.</td><td>0.098<br>0</td><td>0.516</td><td>v.d.</td><td>0.6</td><td>113</td><td>0.5</td><td>1.5</td><td>453</td><td>528</td></tr><tr><td>12LDX40-2</td><td>Qz1</td><td>12.0</td><td>37.7</td><td>66.7</td><td>6.78</td><td>&lt;97.70</td><td>15.4</td><td>1.01</td><td>v.d.</td><td>0.610</td><td>&lt;1.05</td><td>0.285</td><td>1.49</td><td>1.24</td><td>v.d.</td><td>0.387</td><td>1.202</td><td>v.d.</td><td>0.6</td><td>111</td><td>0.5</td><td>1.5</td><td>398</td><td>463</td></tr><tr><td>12LDX40-3</td><td>Qz1</td><td>10.1</td><td>39.0</td><td>65.0</td><td>30.0</td><td>202</td><td>13.7</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.168</td><td>0.98</td><td>1.01</td><td>0.74</td><td>0.226</td><td>0.847</td><td>v.d.</td><td>0.6</td><td>108</td><td>0.5</td><td>1.5</td><td>391</td><td>455</td></tr><tr><td>12LDX40-4</td><td>Qz1</td><td>11.8</td><td>29.4</td><td>73.5</td><td>&lt;3.95</td><td>&lt;75.82</td><td>16.5</td><td>1.241</td><td>v.d.</td><td>1.26</td><td>0.900</td><td>0.191</td><td>1.14</td><td>0.52</td><td>0.214</td><td>0.255</td><td>0.288</td><td>1.40</td><td>0.6</td><td>122</td><td>0.5</td><td>1.5</td><td>402</td><td>468</td></tr></tbody></table>
<table><caption>**Table 4.** LA-ICP-MS trace elements in quartz of the Tongchang porphyry Cu deposit.</caption><thead><tr><th>Spot No.</th><th>CL</th><th>Li</th><th>Na</th><th>Al</th><th>K</th><th>Ca</th><th>Ti</th><th>Mn</th><th>Fe</th><th>Cu</th><th>Zn</th><th>Ga</th><th>Ge</th><th>As</th><th>Sr</th><th>Sn</th><th>Sb</th><th>Pb</th><th>Al Factor</th><th>Al Corr</th><th>P min (kbar)</th><th>P max (kbar)</th><th>Tmin (°C)</th><th>Tmax (°C)</th></tr></thead><tbody><tr><td>12LDX37-1</td><td>Qz1</td><td>9.26</td><td>54.6</td><td>290</td><td>229</td><td>&lt;86.01</td><td>43.2</td><td>1.72</td><td>v.d.</td><td>1.00</td><td>0.78</td><td>0.205</td><td>1.10</td><td>0.490</td><td>1.03</td><td>0.13</td><td>1.59</td><td>1.35</td><td>0.7</td><td>414</td><td>0.5</td><td>1.5</td><td>461</td><td>538</td></tr><tr><td>12LDX37-2</td><td>Qz1</td><td>11.2</td><td>187</td><td>74.3</td><td>49.2</td><td>&lt;39.88</td><td>38.0</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.0207</td><td>1.28</td><td>0.304</td><td>0.31</td><td>0.119</td><td>0.792</td><td>v.d.</td><td>0.7</td><td>106</td><td>0.5</td><td>1.5</td><td>453</td><td>528</td></tr><tr><td>12LDX37-7</td><td>Qz1</td><td>10.6</td><td>v.d.</td><td>65.5</td><td>v.d.</td><td>v.d.</td><td>43.4</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>1.36</td><td>v.d.</td><td>v.d.</td><td>0.100</td><td>0.773</td><td>v.d.</td><td>0.7</td><td>93.6</td><td>0.5</td><td>1.5</td><td>462</td><td>538</td></tr><tr><td>12LDX37-8</td><td>Qz1</td><td>10.0</td><td>120</td><td>134</td><td>104</td><td>&lt;88.69</td><td>35.0</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.0440</td><td>0.83<br>1</td><td>0.350</td><td>0.39</td><td>&lt;0.06<br>2</td><td>0.587</td><td>2.57</td><td>0.7</td><td>191</td><td>0.5</td><td>1.5</td><td>448</td><td>522</td></tr><tr><td>12LDX37-9</td><td>Qz1</td><td>10.8</td><td>689</td><td>74.3</td><td>v.d.</td><td>v.d.</td><td>29.7</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.399</td><td>v.d.</td><td>0.142</td><td>0.467</td><td>v.d.</td><td>0.7</td><td>106</td><td>0.5</td><td>1.5</td><td>438</td><td>510</td></tr><tr><td>12LDX37-14</td><td>Qz1</td><td>6.59</td><td>v.d.</td><td>118</td><td>56.9</td><td>240</td><td>30.5</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.0270</td><td>0.87<br>0</td><td>&lt;0.43</td><td>1.16</td><td>0.207</td><td>v.d.</td><td>v.d.</td><td>0.7</td><td>168</td><td>0.5</td><td>1.5</td><td>439</td><td>512</td></tr><tr><td>12LDX37-15</td><td>Qz1</td><td>7.32</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>109</td><td>35.9</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.0310</td><td>1.1</td><td>0.670</td><td>v.d.</td><td>0.098</td><td>0.561</td><td>v.d.</td><td>0.7</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>450</td><td>524</td></tr><tr><td>12LDX37-36</td><td>Qz1</td><td>13.5</td><td>18.1</td><td>176<br>2</td><td>599</td><td>445</td><td>36.7</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>&lt;1.01</td><td>0.346</td><td>1.41</td><td>0.420</td><td>2.56</td><td>0.054<br>0</td><td>0.378</td><td>0.116</td><td>0.7</td><td>2518</td><td>0.5</td><td>1.5</td><td>451</td><td>525</td></tr><tr><td>12LDX37-34</td><td>Qz1</td><td>7.30</td><td>&lt;2.7<br>1</td><td>135</td><td>28.17</td><td>234</td><td>28.8</td><td>0.711</td><td>v.d.</td><td>1.01</td><td>&lt;0.94</td><td>0.223</td><td>1.31</td><td>0.680</td><td>0.171</td><td>&lt;0.07<br>9</td><td>&lt;0.08<br>0</td><td>0.227</td><td>0.7</td><td>192</td><td>0.5</td><td>1.5</td><td>436</td><td>507</td></tr><tr><td>12LDX37-40</td><td>Qz1</td><td>10.3</td><td>&lt;3.7<br>8</td><td>87.1</td><td>&lt;6.91</td><td>&lt;140.4<br>5</td><td>43.9</td><td>0.144</td><td>2.26</td><td>0.730</td><td>1.65</td><td>0.107</td><td>0.86<br>0</td><td>0.580</td><td>0.221</td><td>&lt;0.08<br>8</td><td>&lt;0.06<br>7</td><td>0.09</td><td>0.7</td><td>124</td><td>0.5</td><td>1.5</td><td>463</td><td>539</td></tr><tr><td>12LDX37-42</td><td>Qz1</td><td>10.2</td><td>141</td><td>70.6</td><td>60.8</td><td>v.d.</td><td>32.3</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.216</td><td>1.58</td><td>0.360</td><td>v.d.</td><td>0.240</td><td>0.199</td><td>1.85</td><td>0.7</td><td>101</td><td>0.5</td><td>1.5</td><td>443</td><td>516</td></tr><tr><td>12LDX37-43</td><td>Qz1</td><td>7.84</td><td>18.9</td><td>58.8</td><td>5.13</td><td>&lt;88.42</td><td>23.2</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.950</td><td>0.247</td><td>1.13</td><td>&lt;0.33</td><td>0.587</td><td>&lt;0.08<br>3</td><td>0.317</td><td>1.02</td><td>0.7</td><td>84.0</td><td>0.5</td><td>1.5</td><td>422</td><td>492</td></tr><tr><td>12LDX37-44</td><td>Qz1</td><td>10.5</td><td>v.d.</td><td>61.3</td><td>v.d.</td><td>457</td><td>24.5</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.079</td><td>1.06</td><td>0.270</td><td>v.d.</td><td>0.162</td><td>0.098</td><td>v.d.</td><td>0.7</td><td>87.6</td><td>0.5</td><td>1.5</td><td>426</td><td>496</td></tr><tr><td>12LDX37-45</td><td>Qz1</td><td>11.3</td><td>&lt;2.9<br>0</td><td>88.8</td><td>&lt;5.24</td><td>&lt;103.2<br>6</td><td>24.9</td><td>0.143</td><td>4.14</td><td>&lt;0.31</td><td>1.50</td><td>0.143</td><td>0.84<br>0</td><td>&lt;0.28<br>8</td><td>0.054</td><td>&lt;0.08<br>1</td><td>&lt;0.08<br>0</td><td>0.096</td><td>0.7</td><td>127</td><td>0.5</td><td>1.5</td><td>427</td><td>497</td></tr><tr><td>12LDX37-46</td><td>Qz1</td><td>10.8</td><td>6.73</td><td>71.6</td><td>8.02</td><td>&lt;58.04</td><td>32.8</td><td>0.819</td><td>v.d.</td><td>0.418</td><td>&lt;0.67</td><td>&lt;0.013<br>3</td><td>0.97<br>5</td><td>0.239</td><td>1.05</td><td>0.055</td><td>&lt;0.04<br>2</td><td>0.233</td><td>0.7</td><td>102</td><td>0.5</td><td>1.5</td><td>444</td><td>517</td></tr><tr><td>12LDX37-47</td><td>Qz1</td><td>10.3</td><td>8.08</td><td>76.1</td><td>&lt;4.52</td><td>99.3</td><td>24.0</td><td>0.237</td><td>4.18</td><td>0.290</td><td>&lt;0.53</td><td>0.130</td><td>1.19</td><td>&lt;0.33</td><td>0.773</td><td>0.190</td><td>0.206</td><td>0.103</td><td>0.7</td><td>109</td><td>0.5</td><td>1.5</td><td>424</td><td>494</td></tr><tr><td>12LDX37-48</td><td>Qz1</td><td>11.2</td><td>v.d.</td><td>64.4</td><td>69.6</td><td>v.d.</td><td>23.4</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.0620</td><td>0.85<br>0</td><td>&lt;0.35</td><td>v.d.</td><td>0.179</td><td>0.113</td><td>v.d.</td><td>0.7</td><td>91.9</td><td>0.5</td><td>1.5</td><td>423</td><td>492</td></tr><tr><td>12LDX37-49</td><td>Qz1</td><td>10.3</td><td>18.8</td><td>99.5</td><td>&lt;5.31</td><td>591</td><td>36.6</td><td>0.105</td><td>2.38</td><td>&lt;0.34</td><td>1.63</td><td>0.348</td><td>1.50</td><td>0.730</td><td>1.29</td><td>0.095</td><td>0.679</td><td>0.259</td><td>0.7</td><td>142</td><td>0.5</td><td>1.5</td><td>451</td><td>525</td></tr><tr><td>12LDX37-50</td><td>Qz1</td><td>12.6</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>30.5</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.134</td><td>1.20</td><td>1.59</td><td>v.d.</td><td>0.177</td><td>1.68</td><td>v.d.</td><td>0.7</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>439</td><td>512</td></tr><tr><td>12LDX40-1</td><td>Qz1</td><td>12.0</td><td>83.0</td><td>67.6</td><td>28.2</td><td>614</td><td>37.8</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.112</td><td>1.64</td><td>0.640</td><td>v.d.</td><td>0.098<br>0</td><td>0.516</td><td>v.d.</td><td>0.6</td><td>113</td><td>0.5</td><td>1.5</td><td>453</td><td>528</td></tr><tr><td>12LDX40-2</td><td>Qz1</td><td>12.0</td><td>37.7</td><td>66.7</td><td>6.78</td><td>&lt;97.70</td><td>15.4</td><td>1.01</td><td>v.d.</td><td>0.610</td><td>&lt;1.05</td><td>0.285</td><td>1.49</td><td>1.24</td><td>v.d.</td><td>0.387</td><td>1.202</td><td>v.d.</td><td>0.6</td><td>111</td><td>0.5</td><td>1.5</td><td>398</td><td>463</td></tr><tr><td>12LDX40-3</td><td>Qz1</td><td>10.1</td><td>39.0</td><td>65.0</td><td>30.0</td><td>202</td><td>13.7</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.168</td><td>0.98</td><td>1.01</td><td>0.74</td><td>0.226</td><td>0.847</td><td>v.d.</td><td>0.6</td><td>108</td><td>0.5</td><td>1.5</td><td>391</td><td>455</td></tr><tr><td>12LDX40-4</td><td>Qz1</td><td>11.8</td><td>29.4</td><td>73.5</td><td>&lt;3.95</td><td>&lt;75.82</td><td>16.5</td><td>1.241</td><td>v.d.</td><td>1.26</td><td>0.900</td><td>0.191</td><td>1.14</td><td>0.52</td><td>0.214</td><td>0.255</td><td>0.288</td><td>1.40</td><td>0.6</td><td>122</td><td>0.5</td><td>1.5</td><td>402</td><td>468</td></tr></tbody></table>
<table><tr><td>12LDX40-5</td><td>Qz1</td><td>8.14</td><td>47.5</td><td>64.4</td><td>8.45</td><td>&lt;87.48</td><td>9.7</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.252</td><td>1.37</td><td>&lt;0.26</td><td>0.788</td><td>0.109</td><td>0.568</td><td>0.85</td><td>0.6</td><td>107</td><td>0.5</td><td>1.5</td><td>372</td><td>432</td></tr><tr><td>12LDX40-6</td><td>Qz1</td><td>14.1</td><td>21.6</td><td>54.5</td><td>&lt;2.64</td><td>&lt;52.57</td><td>13.8</td><td>0.998</td><td>v.d.</td><td>0.403</td><td>0.910</td><td>0.160</td><td>1.15</td><td>0.260</td><td>1.39</td><td>0.160</td><td>0.732</td><td>0.887</td><td>0.6</td><td>90.9</td><td>0.5</td><td>1.5</td><td>392</td><td>456</td></tr><tr><td>12LDX40-7</td><td>Qz1</td><td>7.17</td><td>117</td><td>53.3</td><td>&lt;3.48</td><td>214</td><td>15.9</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.0450</td><td>0.89<br>1</td><td>0.330</td><td>0.564</td><td>0.156</td><td>0.293</td><td>3.00</td><td>0.6</td><td>88.8</td><td>0.5</td><td>1.5</td><td>400</td><td>465</td></tr><tr><td>12LDX40-8</td><td>Qz1</td><td>7.94</td><td>108</td><td>v.d.</td><td>v.d.</td><td>67.2</td><td>20.0</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.369</td><td>0.84<br>7</td><td>0.340</td><td>0.473</td><td>0.033</td><td>&lt;0.02<br>8</td><td>v.d.</td><td>0.6</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>413</td><td>481</td></tr><tr><td>12LDX40-9</td><td>Qz1</td><td>13.8</td><td>9.40</td><td>61.9</td><td>&lt;2.82</td><td>88.7</td><td>21.4</td><td>0.0530</td><td>v.d.</td><td>0.340</td><td>&lt;0.52</td><td>0.298</td><td>0.96</td><td>1.71</td><td>0.084<br>0</td><td>0.142</td><td>0.683</td><td>0.464</td><td>0.6</td><td>103</td><td>0.5</td><td>1.5</td><td>417</td><td>486</td></tr><tr><td>12LDX40-10</td><td>Qz1</td><td>12.9</td><td>31.8</td><td>53.7</td><td>25.3</td><td>&lt;64.58</td><td>21.4</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.415</td><td>1.66</td><td>0.28</td><td>v.d.</td><td>0.559</td><td>0.839</td><td>v.d.</td><td>0.6</td><td>89.5</td><td>0.5</td><td>1.5</td><td>418</td><td>486</td></tr><tr><td>12LDX40-11</td><td>Qz1</td><td>12.1</td><td>56.4</td><td>73.8</td><td>31.5</td><td>&lt;135.2<br>6</td><td>13.2</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.061</td><td>1.00</td><td>&lt;0.43</td><td>0.137</td><td>0.285</td><td>0.614</td><td>v.d.</td><td>0.6</td><td>123</td><td>0.5</td><td>1.5</td><td>389</td><td>453</td></tr><tr><td>12LDX40-12</td><td>Qz1</td><td>13.3</td><td>64.0</td><td>55.1</td><td>32.4</td><td>&lt;58.82</td><td>17.6</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.321</td><td>0.96<br>2</td><td>1.12</td><td>0.036</td><td>0.103</td><td>0.681</td><td>v.d.</td><td>0.6</td><td>91.9</td><td>0.5</td><td>1.5</td><td>406</td><td>472</td></tr><tr><td>12LDX40-13</td><td>Qz1</td><td>12.6</td><td>34.8</td><td>56.9</td><td>22.1</td><td>&lt;80.39</td><td>15.4</td><td>0.838</td><td>4.08</td><td>1.23</td><td>v.d.</td><td>0.245</td><td>1.49</td><td>0.520</td><td>0.093<br>7</td><td>0.783</td><td>0.26</td><td>v.d.</td><td>0.6</td><td>94.8</td><td>0.5</td><td>1.5</td><td>398</td><td>463</td></tr><tr><td>12LDX40-14</td><td>Qz1</td><td>14.6</td><td>29.1</td><td>73.6</td><td>26.8</td><td>138</td><td>10.6</td><td>1.55</td><td>v.d.</td><td>&lt;0.23</td><td>8.82</td><td>0.226</td><td>1.31</td><td>0.530</td><td>0.746</td><td>&lt;0.06<br>2</td><td>0.296</td><td>v.d.</td><td>0.6</td><td>123</td><td>0.5</td><td>1.5</td><td>377</td><td>438</td></tr><tr><td>12LDX40-15</td><td>Qz1</td><td>12.8</td><td>v.d.</td><td>90.1</td><td>56.1</td><td>&lt;55.79</td><td>18.7</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.135</td><td>1.25</td><td>1.78</td><td>0.601</td><td>0.514</td><td>0.79</td><td>v.d.</td><td>0.6</td><td>150</td><td>0.5</td><td>1.5</td><td>409</td><td>476</td></tr><tr><td>12LDX40-16</td><td>Qz1</td><td>15.6</td><td>18.4</td><td>94.5</td><td>8.78</td><td>&lt;128.3<br>2</td><td>27.0</td><td>0.152</td><td>3.88</td><td>1.56</td><td>&lt;1.10</td><td>1.39</td><td>1.11</td><td>2.51</td><td>0.459</td><td>0.231</td><td>0.467</td><td>v.d.</td><td>0.6</td><td>157</td><td>0.5</td><td>1.5</td><td>432</td><td>503</td></tr><tr><td>12LDX40-17</td><td>Qz1</td><td>16.3</td><td>10.5</td><td>71.5</td><td>9.96</td><td>&lt;98.31</td><td>28.6</td><td>0.312</td><td>5.13</td><td>1.83</td><td>2.75</td><td>0.500</td><td>0.94<br>0</td><td>2.38</td><td>v.d.</td><td>0.446</td><td>1.73</td><td>v.d.</td><td>0.6</td><td>119</td><td>0.5</td><td>1.5</td><td>435</td><td>507</td></tr><tr><td>12LDX40-18</td><td>Qz1</td><td>12.3</td><td>104</td><td>66.6</td><td>36.6</td><td>201</td><td>24.5</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.238</td><td>1.46</td><td>0.780</td><td>v.d.</td><td>1.06</td><td>1.47</td><td>v.d.</td><td>0.6</td><td>111</td><td>0.5</td><td>1.5</td><td>426</td><td>496</td></tr><tr><td>12LDX40-19</td><td>Qz1</td><td>17.4</td><td>50.4</td><td>78.9</td><td>22.9</td><td>162</td><td>42.6</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.098</td><td>1.07</td><td>1.59</td><td>1.44</td><td>0.537</td><td>1.51</td><td>v.d.</td><td>0.6</td><td>131</td><td>0.5</td><td>1.5</td><td>461</td><td>537</td></tr><tr><td>12LDX40-20</td><td>Qz1</td><td>13.8</td><td>&lt;2.3<br>0</td><td>61.7</td><td>5.52</td><td>v.d.</td><td>15.4</td><td>&lt;0.037</td><td>2.57</td><td>0.48</td><td>&lt;0.42</td><td>0.437</td><td>0.91</td><td>0.510</td><td>1.12</td><td>0.147</td><td>0.146</td><td>1.7</td><td>0.6</td><td>103</td><td>0.5</td><td>1.5</td><td>398</td><td>463</td></tr><tr><td>12LDX40-21</td><td>Qz1</td><td>14.9</td><td>18.6</td><td>64.6</td><td>11.0</td><td>&lt;65.02</td><td>13.1</td><td>1.26</td><td>v.d.</td><td>1.07</td><td>1.88</td><td>0.160</td><td>1.02</td><td>1.7</td><td>v.d.</td><td>0.257</td><td>0.233</td><td>1.49</td><td>0.6</td><td>108</td><td>0.5</td><td>1.5</td><td>389</td><td>452</td></tr><tr><td>12LDX40-22</td><td>Qz1</td><td>11.2</td><td>59.2</td><td>52.8</td><td>19.3</td><td>&lt;92.12</td><td>16.0</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.510</td><td>1.00</td><td>0.720</td><td>0.645</td><td>0.191</td><td>0.130</td><td>v.d.</td><td>0.6</td><td>88</td><td>0.5</td><td>1.5</td><td>400</td><td>466</td></tr><tr><td>12LDX40-23</td><td>Qz1</td><td>11.8</td><td>18.5</td><td>77.5</td><td>&lt;4.66</td><td>&lt;79.06</td><td>14.2</td><td>0.138</td><td>3.77</td><td>0.270</td><td>&lt;0.48</td><td>0.253</td><td>1.38</td><td>0.580</td><td>0.163</td><td>0.095</td><td>0.283</td><td>0.307</td><td>0.6</td><td>129</td><td>0.5</td><td>1.5</td><td>393</td><td>457</td></tr><tr><td>12LDX40-24</td><td>Qz1</td><td>13.6</td><td>40.5</td><td>67.6</td><td>13.1</td><td>&lt;74.70</td><td>24.7</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.221</td><td>1.11</td><td>0.560</td><td>0.058</td><td>0.118</td><td>0.15</td><td>v.d.</td><td>0.6</td><td>113</td><td>0.5</td><td>1.5</td><td>426</td><td>496</td></tr><tr><td>12LDX40-25</td><td>Qz1</td><td>8.41</td><td>56.5</td><td>v.d.</td><td>137</td><td>105</td><td>16.7</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.203</td><td>1.30</td><td>0.670</td><td>v.d.</td><td>0.093</td><td>&lt;0.06<br>3</td><td>0.734</td><td>0.6</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>403</td><td>469</td></tr><tr><td>10DX328-13</td><td>Qz1</td><td>7.24</td><td>41.5</td><td>57.2</td><td>4.37</td><td>151</td><td>33.1</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>&lt;0.77</td><td>0.424</td><td>1.40</td><td>0.300</td><td>v.d.</td><td>0.128</td><td>0.151</td><td>0.911</td><td>0.76</td><td>75.3</td><td>0.5</td><td>1.5</td><td>444</td><td>517</td></tr><tr><td>10DX328-14</td><td>Qz1</td><td>8.40</td><td>97.7</td><td>58.3</td><td>&lt;4.11</td><td>v.d.</td><td>37.8</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>&lt;0.86</td><td>0.102</td><td>1.98</td><td>0.880</td><td>v.d.</td><td>0.151</td><td>0.116</td><td>0.603</td><td>0.76</td><td>76.6</td><td>0.5</td><td>1.5</td><td>453</td><td>528</td></tr><tr><td>10DX328-16</td><td>Qz1</td><td>13.4</td><td>117</td><td>73.0</td><td>13.6</td><td>&lt;79.63</td><td>31.4</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>2.93</td><td>1.31</td><td>0.099</td><td>1.78</td><td>0.360</td><td>v.d.</td><td>0.144</td><td>0.058</td><td>v.d.</td><td>0.76</td><td>96.1</td><td>0.5</td><td>1.5</td><td>441</td><td>514</td></tr><tr><td>10DX328-35</td><td>Qz1</td><td>13.2</td><td>118</td><td>71.1</td><td>32.0</td><td>&lt;68.97</td><td>28.4</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>3.92</td><td>0.098</td><td>1.33</td><td>0.175</td><td>0.194</td><td>0.096</td><td>0.346</td><td>v.d.</td><td>0.76</td><td>93.5</td><td>0.5</td><td>1.5</td><td>435</td><td>506</td></tr><tr><td>10DX328-36</td><td>Qz1</td><td>11.5</td><td>133</td><td>60.5</td><td>18.4</td><td>v.d.</td><td>32.7</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>3.00</td><td>0.524</td><td>2.15</td><td>1.35</td><td>v.d.</td><td>0.451</td><td>0.304</td><td>v.d.</td><td>0.76</td><td>79.5</td><td>0.5</td><td>1.5</td><td>444</td><td>517</td></tr></table>
<table>
  <tr>
    <td>12LDX40-5</td>
    <td>Qz1</td>
    <td>8.14</td>
    <td>47.5</td>
    <td>64.4</td>
    <td>8.45</td>
    <td>&lt;87.48</td>
    <td>9.7</td>
    <td>v.d.</td>
    <td>v.d.</td>
    <td>v.d.</td>
    <td>v.d.</td>
    <td>0.252</td>
    <td>1.37</td>
    <td>&lt;0.26</td>
    <td>0.788</td>
    <td>0.109</td>
    <td>0.568</td>
    <td>0.85</td>
    <td>0.6</td>
    <td>107</td>
    <td>0.5</td>
    <td>1.5</td>
    <td>372</td>
    <td>432</td>
  </tr>
  <tr>
    <td>12LDX40-6</td>
    <td>Qz1</td>
    <td>14.1</td>
    <td>21.6</td>
    <td>54.5</td>
    <td>&lt;2.64</td>
    <td>&lt;52.57</td>
    <td>13.8</td>
    <td>0.998</td>
    <td>v.d.</td>
    <td>0.403</td>
    <td>0.910</td>
    <td>0.160</td>
    <td>1.15</td>
    <td>0.260</td>
    <td>1.39</td>
    <td>0.160</td>
    <td>0.732</td>
    <td>0.887</td>
    <td>0.6</td>
    <td>90.9</td>
    <td>0.5</td>
    <td>1.5</td>
    <td>392</td>
    <td>456</td>
  </tr>
  <tr>
    <td>12LDX40-7</td>
    <td>Qz1</td>
    <td>7.17</td>
    <td>117</td>
    <td>53.3</td>
    <td>&lt;3.48</td>
    <td>214</td>
    <td>15.9</td>
    <td>v.d.</td>
    <td>v.d.</td>
    <td>v.d.</td>
    <td>v.d.</td>
    <td>0.0450</td>
    <td>0.89<br>1</td>
    <td>0.330</td>
    <td>0.564</td>
    <td>0.156</td>
    <td>0.293</td>
    <td>3.00</td>
    <td>0.6</td>
    <td>88.8</td>
    <td>0.5</td>
    <td>1.5</td>
    <td>400</td>
    <td>465</td>
  </tr>
  <tr>
    <td>12LDX40-8</td>
    <td>Qz1</td>
    <td>7.94</td>
    <td>108</td>
    <td>v.d.</td>
    <td>v.d.</td>
    <td>67.2</td>
    <td>20.0</td>
    <td>v.d.</td>
    <td>v.d.</td>
    <td>v.d.</td>
    <td>v.d.</td>
    <td>0.369</td>
    <td>0.84<br>7</td>
    <td>0.340</td>
    <td>0.473</td>
    <td>0.033</td>
    <td>&lt;0.02<br>8</td>
    <td>v.d.</td>
    <td>0.6</td>
    <td>v.d.</td>
    <td>0.5</td>
    <td>1.5</td>
    <td>413</td>
    <td>481</td>
  </tr>
  <tr>
    <td>12LDX40-9</td>
    <td>Qz1</td>
    <td>13.8</td>
    <td>9.40</td>
    <td>61.9</td>
    <td>&lt;2.82</td>
    <td>88.7</td>
    <td>21.4</td>
    <td>0.0530</td>
    <td>v.d.</td>
    <td>0.340</td>
    <td>&lt;0.52</td>
    <td>0.298</td>
    <td>0.96</td>
    <td>1.71</td>
    <td>0.084<br>0</td>
    <td>0.142</td>
    <td>0.683</td>
    <td>0.464</td>
    <td>0.6</td>
    <td>103</td>
    <td>0.5</td>
    <td>1.5</td>
    <td>417</td>
    <td>486</td>
  </tr>
  <tr>
    <td>12LDX40-10</td>
    <td>Qz1</td>
    <td>12.9</td>
    <td>31.8</td>
    <td>53.7</td>
    <td>25.3</td>
    <td>&lt;64.58</td>
    <td>21.4</td>
    <td>v.d.</td>
    <td>v.d.</td>
    <td>v.d.</td>
    <td>v.d.</td>
    <td>0.415</td>
    <td>1.66</td>
    <td>0.28</td>
    <td>v.d.</td>
    <td>0.559</td>
    <td>0.839</td>
    <td>v.d.</td>
    <td>0.6</td>
    <td>89.5</td>
    <td>0.5</td>
    <td>1.5</td>
    <td>418</td>
    <td>486</td>
  </tr>
  <tr>
    <td>12LDX40-11</td>
    <td>Qz1</td>
    <td>12.1</td>
    <td>56.4</td>
    <td>73.8</td>
    <td>31.5</td>
    <td>&lt;135.2<br>6</td>
    <td>13.2</td>
    <td>v.d.</td>
    <td>v.d.</td>
    <td>v.d.</td>
    <td>v.d.</td>
    <td>0.061</td>
    <td>1.00</td>
    <td>&lt;0.43</td>
    <td>0.137</td>
    <td>0.285</td>
    <td>0.614</td>
    <td>v.d.</td>
    <td>0.6</td>
    <td>123</td>
    <td>0.5</td>
    <td>1.5</td>
    <td>389</td>
    <td>453</td>
  </tr>
  <tr>
    <td>12LDX40-12</td>
    <td>Qz1</td>
    <td>13.3</td>
    <td>64.0</td>
    <td>55.1</td>
    <td>32.4</td>
    <td>&lt;58.82</td>
    <td>17.6</td>
    <td>v.d.</td>
    <td>v.d.</td>
    <td>v.d.</td>
    <td>v.d.</td>
    <td>0.321</td>
    <td>0.96<br>2</td>
    <td>1.12</td>
    <td>0.036</td>
    <td>0.103</td>
    <td>0.681</td>
    <td>v.d.</td>
    <td>0.6</td>
    <td>91.9</td>
    <td>0.5</td>
    <td>1.5</td>
    <td>406</td>
    <td>472</td>
  </tr>
  <tr>
    <td>12LDX40-13</td>
    <td>Qz1</td>
    <td>12.6</td>
    <td>34.8</td>
    <td>56.9</td>
    <td>22.1</td>
    <td>&lt;80.39</td>
    <td>15.4</td>
    <td>0.838</td>
    <td>4.08</td>
    <td>1.23</td>
    <td>v.d.</td>
    <td>0.245</td>
    <td>1.49</td>
    <td>0.520</td>
    <td>0.093<br>7</td>
    <td>0.783</td>
    <td>0.26</td>
    <td>v.d.</td>
    <td>0.6</td>
    <td>94.8</td>
    <td>0.5</td>
    <td>1.5</td>
    <td>398</td>
    <td>463</td>
  </tr>
  <tr>
    <td>12LDX40-14</td>
    <td>Qz1</td>
    <td>14.6</td>
    <td>29.1</td>
    <td>73.6</td>
    <td>26.8</td>
    <td>138</td>
    <td>10.6</td>
    <td>1.55</td>
    <td>v.d.</td>
    <td>&lt;0.23</td>
    <td>8.82</td>
    <td>0.226</td>
    <td>1.31</td>
    <td>0.530</td>
    <td>0.746</td>
    <td>&lt;0.06<br>2</td>
    <td>0.296</td>
    <td>v.d.</td>
    <td>0.6</td>
    <td>123</td>
    <td>0.5</td>
    <td>1.5</td>
    <td>377</td>
    <td>438</td>
  </tr>
  <tr>
    <td>12LDX40-15</td>
    <td>Qz1</td>
    <td>12.8</td>
    <td>v.d.</td>
    <td>90.1</td>
    <td>56.1</td>
    <td>&lt;55.79</td>
    <td>18.7</td>
    <td>v.d.</td>
    <td>v.d.</td>
    <td>v.d.</td>
    <td>v.d.</td>
    <td>0.135</td>
    <td>1.25</td>
    <td>1.78</td>
    <td>0.601</td>
    <td>0.514</td>
    <td>0.79</td>
    <td>v.d.</td>
    <td>0.6</td>
    <td>150</td>
    <td>0.5</td>
    <td>1.5</td>
    <td>409</td>
    <td>476</td>
  </tr>
  <tr>
    <td>12LDX40-16</td>
    <td>Qz1</td>
    <td>15.6</td>
    <td>18.4</td>
    <td>94.5</td>
    <td>8.78</td>
    <td>&lt;128.3<br>2</td>
    <td>27.0</td>
    <td>0.152</td>
    <td>3.88</td>
    <td>1.56</td>
    <td>&lt;1.10</td>
    <td>1.39</td>
    <td>1.11</td>
    <td>2.51</td>
    <td>0.459</td>
    <td>0.231</td>
    <td>0.467</td>
    <td>v.d.</td>
    <td>0.6</td>
    <td>157</td>
    <td>0.5</td>
    <td>1.5</td>
    <td>432</td>
    <td>503</td>
  </tr>
  <tr>
    <td>12LDX40-17</td>
    <td>Qz1</td>
    <td>16.3</td>
    <td>10.5</td>
    <td>71.5</td>
    <td>9.96</td>
    <td>&lt;98.31</td>
    <td>28.6</td>
    <td>0.312</td>
    <td>5.13</td>
    <td>1.83</td>
    <td>2.75</td>
    <td>0.500</td>
    <td>0.94<br>0</td>
    <td>2.38</td>
    <td>v.d.</td>
    <td>0.446</td>
    <td>1.73</td>
    <td>v.d.</td>
    <td>0.6</td>
    <td>119</td>
    <td>0.5</td>
    <td>1.5</td>
    <td>435</td>
    <td>507</td>
  </tr>
  <tr>
    <td>12LDX40-18</td>
    <td>Qz1</td>
    <td>12.3</td>
    <td>104</td>
    <td>66.6</td>
    <td>36.6</td>
    <td>201</td>
    <td>24.5</td>
    <td>v.d.</td>
    <td>v.d.</td>
    <td>v.d.</td>
    <td>v.d.</td>
    <td>0.238</td>
    <td>1.46</td>
    <td>0.780</td>
    <td>v.d.</td>
    <td>1.06</td>
    <td>1.47</td>
    <td>v.d.</td>
    <td>0.6</td>
    <td>111</td>
    <td>0.5</td>
    <td>1.5</td>
    <td>426</td>
    <td>496</td>
  </tr>
  <tr>
    <td>12LDX40-19</td>
    <td>Qz1</td>
    <td>17.4</td>
    <td>50.4</td>
    <td>78.9</td>
    <td>22.9</td>
    <td>162</td>
    <td>42.6</td>
    <td>v.d.</td>
    <td>v.d.</td>
    <td>v.d.</td>
    <td>v.d.</td>
    <td>0.098</td>
    <td>1.07</td>
    <td>1.59</td>
    <td>1.44</td>
    <td>0.537</td>
    <td>1.51</td>
    <td>v.d.</td>
    <td>0.6</td>
    <td>131</td>
    <td>0.5</td>
    <td>1.5</td>
    <td>461</td>
    <td>537</td>
  </tr>
  <tr>
    <td>12LDX40-20</td>
    <td>Qz1</td>
    <td>13.8</td>
    <td>&lt;2.3<br>0</td>
    <td>61.7</td>
    <td>5.52</td>
    <td>v.d.</td>
    <td>15.4</td>
    <td>&lt;0.037</td>
    <td>2.57</td>
    <td>0.48</td>
    <td>&lt;0.42</td>
    <td>0.437</td>
    <td>0.91</td>
    <td>0.510</td>
    <td>1.12</td>
    <td>0.147</td>
    <td>0.146</td>
    <td>1.7</td>
    <td>0.6</td>
    <td>103</td>
    <td>0.5</td>
    <td>1.5</td>
    <td>398</td>
    <td>463</td>
  </tr>
  <tr>
    <td>12LDX40-21</td>
    <td>Qz1</td>
    <td>14.9</td>
    <td>18.6</td>
    <td>64.6</td>
    <td>11.0</td>
    <td>&lt;65.02</td>
    <td>13.1</td>
    <td>1.26</td>
    <td>v.d.</td>
    <td>1.07</td>
    <td>1.88</td>
    <td>0.160</td>
    <td>1.02</td>
    <td>1.7</td>
    <td>v.d.</td>
    <td>0.257</td>
    <td>0.233</td>
    <td>1.49</td>
    <td>0.6</td>
    <td>108</td>
    <td>0.5</td>
    <td>1.5</td>
    <td>389</td>
    <td>452</td>
  </tr>
  <tr>
    <td>12LDX40-22</td>
    <td>Qz1</td>
    <td>11.2</td>
    <td>59.2</td>
    <td>52.8</td>
    <td>19.3</td>
    <td>&lt;92.12</td>
    <td>16.0</td>
    <td>v.d.</td>
    <td>v.d.</td>
    <td>v.d.</td>
    <td>v.d.</td>
    <td>0.510</td>
    <td>1.00</td>
    <td>0.720</td>
    <td>0.645</td>
    <td>0.191</td>
    <td>0.130</td>
    <td>v.d.</td>
    <td>0.6</td>
    <td>88</td>
    <td>0.5</td>
    <td>1.5</td>
    <td>400</td>
    <td>466</td>
  </tr>
  <tr>
    <td>12LDX40-23</td>
    <td>Qz1</td>
    <td>11.8</td>
    <td>18.5</td>
    <td>77.5</td>
    <td>&lt;4.66</td>
    <td>&lt;79.06</td>
    <td>14.2</td>
    <td>0.138</td>
    <td>3.77</td>
    <td>0.270</td>
    <td>&lt;0.48</td>
    <td>0.253</td>
    <td>1.38</td>
    <td>0.580</td>
    <td>0.163</td>
    <td>0.095</td>
    <td>0.283</td>
    <td>0.307</td>
    <td>0.6</td>
    <td>129</td>
    <td>0.5</td>
    <td>1.5</td>
    <td>393</td>
    <td>457</td>
  </tr>
  <tr>
    <td>12LDX40-24</td>
    <td>Qz1</td>
    <td>13.6</td>
    <td>40.5</td>
    <td>67.6</td>
    <td>13.1</td>
    <td>&lt;74.70</td>
    <td>24.7</td>
    <td>v.d.</td>
    <td>v.d.</td>
    <td>v.d.</td>
    <td>v.d.</td>
    <td>0.221</td>
    <td>1.11</td>
    <td>0.560</td>
    <td>0.058</td>
    <td>0.118</td>
    <td>0.15</td>
    <td>v.d.</td>
    <td>0.6</td>
    <td>113</td>
    <td>0.5</td>
    <td>1.5</td>
    <td>426</td>
    <td>496</td>
  </tr>
  <tr>
    <td>12LDX40-25</td>
    <td>Qz1</td>
    <td>8.41</td>
    <td>56.5</td>
    <td>v.d.</td>
    <td>137</td>
    <td>105</td>
    <td>16.7</td>
    <td>v.d.</td>
    <td>v.d.</td>
    <td>v.d.</td>
    <td>v.d.</td>
    <td>0.203</td>
    <td>1.30</td>
    <td>0.670</td>
    <td>v.d.</td>
    <td>0.093</td>
    <td>&lt;0.06<br>3</td>
    <td>0.734</td>
    <td>0.6</td>
    <td>v.d.</td>
    <td>0.5</td>
    <td>1.5</td>
    <td>403</td>
    <td>469</td>
  </tr>
  <tr>
    <td>10DX328-13</td>
    <td>Qz1</td>
    <td>7.24</td>
    <td>41.5</td>
    <td>57.2</td>
    <td>4.37</td>
    <td>151</td>
    <td>33.1</td>
    <td>v.d.</td>
    <td>v.d.</td>
    <td>v.d.</td>
    <td>v.d.</td>
    <td>&lt;0.77</td>
    <td>0.424</td>
    <td>1.40</td>
    <td>0.300</td>
    <td>v.d.</td>
    <td>0.128</td>
    <td>0.151</td>
    <td>0.911</td>
    <td>0.76</td>
    <td>75.3</td>
    <td>0.5</td>
    <td>1.5</td>
    <td>444</td>
    <td>517</td>
  </tr>
  <tr>
    <td>10DX328-14</td>
    <td>Qz1</td>
    <td>8.40</td>
    <td>97.7</td>
    <td>58.3</td>
    <td>&lt;4.11</td>
    <td>v.d.</td>
    <td>37.8</td>
    <td>v.d.</td>
    <td>v.d.</td>
    <td>v.d.</td>
    <td>v.d.</td>
    <td>&lt;0.86</td>
    <td>0.102</td>
    <td>1.98</td>
    <td>0.880</td>
    <td>v.d.</td>
    <td>0.151</td>
    <td>0.116</td>
    <td>0.603</td>
    <td>0.76</td>
    <td>76.6</td>
    <td>0.5</td>
    <td>1.5</td>
    <td>453</td>
    <td>528</td>
  </tr>
  <tr>
    <td>10DX328-16</td>
    <td>Qz1</td>
    <td>13.4</td>
    <td>117</td>
    <td>73.0</td>
    <td>13.6</td>
    <td>&lt;79.63</td>
    <td>31.4</td>
    <td>v.d.</td>
    <td>v.d.</td>
    <td>v.d.</td>
    <td>v.d.</td>
    <td>2.93</td>
    <td>1.31</td>
    <td>0.099</td>
    <td>1.78</td>
    <td>0.360</td>
    <td>v.d.</td>
    <td>0.144</td>
    <td>0.058</td>
    <td>v.d.</td>
    <td>0.76</td>
    <td>96.1</td>
    <td>0.5</td>
    <td>1.5</td>
    <td>441</td>
    <td>514</td>
  </tr>
  <tr>
    <td>10DX328-35</td>
    <td>Qz1</td>
    <td>13.2</td>
    <td>118</td>
    <td>71.1</td>
    <td>32.0</td>
    <td>&lt;68.97</td>
    <td>28.4</td>
    <td>v.d.</td>
    <td>v.d.</td>
    <td>v.d.</td>
    <td>v.d.</td>
    <td>3.92</td>
    <td>0.098</td>
    <td>1.33</td>
    <td>0.175</td>
    <td>0.194</td>
    <td>0.096</td>
    <td>0.346</td>
    <td>v.d.</td>
    <td>0.76</td>
    <td>93.5</td>
    <td>0.5</td>
    <td>1.5</td>
    <td>435</td>
    <td>506</td>
  </tr>
  <tr>
    <td>10DX328-36</td>
    <td>Qz1</td>
    <td>11.5</td>
    <td>133</td>
    <td>60.5</td>
    <td>18.4</td>
    <td>v.d.</td>
    <td>32.7</td>
    <td>v.d.</td>
    <td>v.d.</td>
    <td>v.d.</td>
    <td>v.d.</td>
    <td>3.00</td>
    <td>0.524</td>
    <td>2.15</td>
    <td>1.35</td>
    <td>v.d.</td>
    <td>0.451</td>
    <td>0.304</td>
    <td>v.d.</td>
    <td>0.76</td>
    <td>79.5</td>
    <td>0.5</td>
    <td>1.5</td>
    <td>444</td>
    <td>517</td>
  </tr>
</table>
<table><tr><td>10DX328-37</td><td>Qz1</td><td>7.15</td><td>25.0</td><td>83.1</td><td>8.2</td><td>&lt;74.08</td><td>31.1</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>&lt;0.77</td><td>0.229</td><td>1.24</td><td>0.310</td><td>v.d.</td><td>0.101</td><td>0.263</td><td>0.651</td><td>0.76</td><td>109</td><td>0.5</td><td>1.5</td><td>441</td><td>513</td></tr><tr><td>10DX261-12</td><td>Qz1</td><td>12.5</td><td>11.0</td><td>124</td><td>29.2</td><td>&lt;51.06</td><td>43.0</td><td>0.313</td><td>v.d.</td><td>v.d.</td><td>&lt;0.39</td><td>0.116</td><td>0.90<br>9</td><td>0.367</td><td>v.d.</td><td>1.81</td><td>0.257</td><td>0.097</td><td>0.62</td><td>163</td><td>0.5</td><td>1.5</td><td>461</td><td>537</td></tr><tr><td>10DX261-13</td><td>Qz1</td><td>16.7</td><td>5.42</td><td>v.d.</td><td>62.5</td><td>&lt;67.40</td><td>57.6</td><td>0.336</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.102</td><td>1.45</td><td>&lt;0.22</td><td>2.23</td><td>0.116</td><td>0.210</td><td>v.d.</td><td>0.62</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>480</td><td>560</td></tr><tr><td>10DX261-18</td><td>Qz1</td><td>15.3</td><td>167</td><td>v.d.</td><td>v.d.</td><td>&lt;43.16</td><td>32.0</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.456</td><td>1.40</td><td>0.310</td><td>0.500</td><td>0.077</td><td>0.159</td><td>v.d.</td><td>0.62</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>442</td><td>515</td></tr><tr><td>10DX261-19</td><td>Qz1</td><td>16.7</td><td>35.8</td><td>498</td><td>292</td><td>&lt;55.98</td><td>36.7</td><td>v.d.</td><td>v.d.</td><td>0.492</td><td>v.d.</td><td>0.936</td><td>0.90<br>9</td><td>0.770</td><td>0.987</td><td>0.135</td><td>0.404</td><td>0.612</td><td>0.62</td><td>656</td><td>0.5</td><td>1.5</td><td>451</td><td>525</td></tr><tr><td>10DX261-20</td><td>Qz1</td><td>12.6</td><td>5.48</td><td>67.4</td><td>&lt;3.49</td><td>&lt;69.43</td><td>15.9</td><td>0.705</td><td>6.44</td><td>v.d.</td><td>v.d.</td><td>0.419</td><td>0.73<br>1</td><td>0.740</td><td>0.084</td><td>&lt;0.04<br>9</td><td>0.166</td><td>v.d.</td><td>0.62</td><td>88.6</td><td>0.5</td><td>1.5</td><td>400</td><td>465</td></tr><tr><td>10DX261-26</td><td>Qz1</td><td>12.7</td><td>28.3</td><td>85.7</td><td>15.7</td><td>229</td><td>19.1</td><td>0.300</td><td>6.27</td><td>0.620</td><td>v.d.</td><td>0.795</td><td>1.69</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.62</td><td>113</td><td>0.5</td><td>1.5</td><td>411</td><td>478</td></tr><tr><td>10DX261-29</td><td>Qz1</td><td>11.5</td><td>96.5</td><td>84.2</td><td>25.8</td><td>&lt;74.43</td><td>34.3</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>1.12</td><td>0.166</td><td>10.4</td><td>0.070<br>0</td><td>0.292</td><td>v.d.</td><td>0.62</td><td>111</td><td>0.5</td><td>1.5</td><td>447</td><td>520</td></tr><tr><td>10DX261-28</td><td>Qz1</td><td>10.2</td><td>51.2</td><td>104</td><td>36.8</td><td>&lt;89.38</td><td>22.3</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.793</td><td>1.40</td><td>0.430</td><td>0.844</td><td>0.188</td><td>0.914</td><td>0.731</td><td>0.62</td><td>137</td><td>0.5</td><td>1.5</td><td>420</td><td>489</td></tr><tr><td>10DX261-34</td><td>Qz1</td><td>12.7</td><td>&lt;2.5<br>8</td><td>120</td><td>23.4</td><td>89.0</td><td>21.7</td><td>0.226</td><td>v.d.</td><td>v.d.</td><td>1.22</td><td>0.348</td><td>1.29</td><td>0.390</td><td>0.180</td><td>0.087<br>0</td><td>0.189</td><td>0.36</td><td>0.62</td><td>158</td><td>0.5</td><td>1.5</td><td>418</td><td>487</td></tr><tr><td>12DXF05-5</td><td>Qz2<br>a</td><td>13.9</td><td>16.5</td><td>75.7</td><td>&lt;6.89</td><td>204</td><td>152</td><td>1.43</td><td>7.93</td><td>0.730</td><td>&lt;1.68</td><td>0.155</td><td>1.09</td><td>0.390</td><td>0.832</td><td>&lt;0.09<br>8</td><td>&lt;0.09<br>0</td><td>0.296</td><td>0.52</td><td>146</td><td>0.5</td><td>1.5</td><td>543</td><td>635</td></tr><tr><td>12DXF05-6</td><td>Qz2<br>a</td><td>14.8</td><td>25.5</td><td>59.2</td><td>&lt;3.92</td><td>&lt;75.23</td><td>56.9</td><td>1.32</td><td>7.42</td><td>0.202</td><td>0.550</td><td>0.171</td><td>1.10</td><td>&lt;0.18<br>8</td><td>1.41</td><td>0.057<br>0</td><td>&lt;0.05<br>7</td><td>0.491</td><td>0.52</td><td>114</td><td>0.5</td><td>1.5</td><td>479</td><td>559</td></tr><tr><td>12DXF05-7</td><td>Qz2<br>a</td><td>15.9</td><td>v.d.</td><td>207</td><td>108</td><td>215</td><td>193</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.179</td><td>0.64<br>4</td><td>0.920</td><td>1.46</td><td>&lt;0.07<br>2</td><td>0.304</td><td>v.d.</td><td>0.52</td><td>399</td><td>0.5</td><td>1.5</td><td>558</td><td>653</td></tr><tr><td>12DXF05-8</td><td>Qz2<br>a</td><td>15.4</td><td>v.d.</td><td>50.3</td><td>29.4</td><td>&lt;67.91</td><td>165</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.045</td><td>0.81</td><td>0.240</td><td>v.d.</td><td>&lt;0.05<br>4</td><td>0.09</td><td>v.d.</td><td>0.52</td><td>96.8</td><td>0.5</td><td>1.5</td><td>548</td><td>641</td></tr><tr><td>12DXF05-9</td><td>Qz2<br>a</td><td>13.9</td><td>&lt;3.8<br>3</td><td>56.7</td><td>&lt;6.52</td><td>&lt;127.1<br>5</td><td>167</td><td>&lt;0.070</td><td>2.39</td><td>&lt;0.25</td><td>&lt;0.99</td><td>0.133</td><td>0.81</td><td>&lt;0.35</td><td>0.136</td><td>0.219</td><td>&lt;0.07<br>5</td><td>0.979</td><td>0.52</td><td>109</td><td>0.5</td><td>1.5</td><td>549</td><td>643</td></tr><tr><td>12DXF05-10</td><td>Qz2<br>a</td><td>12.8</td><td>v.d.</td><td>53.5</td><td>66.0</td><td>101</td><td>90.6</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.114</td><td>0.75<br>7</td><td>0.233</td><td>v.d.</td><td>&lt;0.04<br>6</td><td>&lt;0.03<br>6</td><td>v.d.</td><td>0.52</td><td>103</td><td>0.5</td><td>1.5</td><td>510</td><td>595</td></tr><tr><td>12DXF05-11</td><td>Qz2<br>a</td><td>13.1</td><td>83.8</td><td>57.9</td><td>7.30</td><td>&lt;72.94</td><td>174</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.195</td><td>1.04</td><td>&lt;0.17<br>1</td><td>1.48</td><td>&lt;0.05<br>8</td><td>&lt;0.05<br>2</td><td>0.939</td><td>0.52</td><td>111</td><td>0.5</td><td>1.5</td><td>552</td><td>645</td></tr><tr><td>12DXF05-12</td><td>Qz2<br>a</td><td>23.3</td><td>71.7</td><td>225</td><td>110</td><td>105.9</td><td>97.6</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.114</td><td>0.87<br>1</td><td>&lt;0.20</td><td>0.349</td><td>0.228</td><td>0.042</td><td>1.29</td><td>0.52</td><td>433</td><td>0.5</td><td>1.5</td><td>515</td><td>601</td></tr><tr><td>12DXF05-13</td><td>Qz2<br>a</td><td>27.2</td><td>9.92</td><td>313</td><td>43.5</td><td>&lt;70.04</td><td>164</td><td>0.657</td><td>v.d.</td><td>&lt;0.13<br>0</td><td>1.25</td><td>0.0620</td><td>0.91<br>1</td><td>&lt;0.14<br>7</td><td>0.369</td><td>0.087</td><td>&lt;0.04<br>5</td><td>0.161</td><td>0.52</td><td>602</td><td>0.5</td><td>1.5</td><td>548</td><td>641</td></tr><tr><td>12DXF05-14</td><td>Qz2<br>a</td><td>17.4</td><td>v.d.</td><td>v.d.</td><td>133</td><td>&lt;84.66</td><td>130</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.0520</td><td>0.65<br>1</td><td>0.306</td><td>v.d.</td><td>&lt;0.06<br>9</td><td>0.057</td><td>v.d.</td><td>0.52</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>533</td><td>623</td></tr><tr><td>12DXF05-15</td><td>Qz2<br>a</td><td>27.5</td><td>49.8</td><td>218</td><td>62.5</td><td>&lt;50.53</td><td>157</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.0490</td><td>0.71<br>9</td><td>&lt;0.09<br>3</td><td>0.233</td><td>0.072</td><td>&lt;0.02<br>4</td><td>0.753</td><td>0.52</td><td>420</td><td>0.5</td><td>1.5</td><td>545</td><td>638</td></tr></table>
<table><tr><td>10DX328-37</td><td>Qz1</td><td>7.15</td><td>25.0</td><td>83.1</td><td>8.2</td><td>&lt;74.08</td><td>31.1</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>&lt;0.77</td><td>0.229</td><td>1.24</td><td>0.310</td><td>v.d.</td><td>0.101</td><td>0.263</td><td>0.651</td><td>0.76</td><td>109</td><td>0.5</td><td>1.5</td><td>441</td><td>513</td></tr><tr><td>10DX261-12</td><td>Qz1</td><td>12.5</td><td>11.0</td><td>124</td><td>29.2</td><td>&lt;51.06</td><td>43.0</td><td>0.313</td><td>v.d.</td><td>v.d.</td><td>&lt;0.39</td><td>0.116</td><td>0.90<br>9</td><td>0.367</td><td>v.d.</td><td>1.81</td><td>0.257</td><td>0.097</td><td>0.62</td><td>163</td><td>0.5</td><td>1.5</td><td>461</td><td>537</td></tr><tr><td>10DX261-13</td><td>Qz1</td><td>16.7</td><td>5.42</td><td>v.d.</td><td>62.5</td><td>&lt;67.40</td><td>57.6</td><td>0.336</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.102</td><td>1.45</td><td>&lt;0.22</td><td>2.23</td><td>0.116</td><td>0.210</td><td>v.d.</td><td>0.62</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>480</td><td>560</td></tr><tr><td>10DX261-18</td><td>Qz1</td><td>15.3</td><td>167</td><td>v.d.</td><td>v.d.</td><td>&lt;43.16</td><td>32.0</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.456</td><td>1.40</td><td>0.310</td><td>0.500</td><td>0.077</td><td>0.159</td><td>v.d.</td><td>0.62</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>442</td><td>515</td></tr><tr><td>10DX261-19</td><td>Qz1</td><td>16.7</td><td>35.8</td><td>498</td><td>292</td><td>&lt;55.98</td><td>36.7</td><td>v.d.</td><td>v.d.</td><td>0.492</td><td>v.d.</td><td>0.936</td><td>0.90<br>9</td><td>0.770</td><td>0.987</td><td>0.135</td><td>0.404</td><td>0.612</td><td>0.62</td><td>656</td><td>0.5</td><td>1.5</td><td>451</td><td>525</td></tr><tr><td>10DX261-20</td><td>Qz1</td><td>12.6</td><td>5.48</td><td>67.4</td><td>&lt;3.49</td><td>&lt;69.43</td><td>15.9</td><td>0.705</td><td>6.44</td><td>v.d.</td><td>v.d.</td><td>0.419</td><td>0.73<br>1</td><td>0.740</td><td>0.084</td><td>&lt;0.04<br>9</td><td>0.166</td><td>v.d.</td><td>0.62</td><td>88.6</td><td>0.5</td><td>1.5</td><td>400</td><td>465</td></tr><tr><td>10DX261-26</td><td>Qz1</td><td>12.7</td><td>28.3</td><td>85.7</td><td>15.7</td><td>229</td><td>19.1</td><td>0.300</td><td>6.27</td><td>0.620</td><td>v.d.</td><td>0.795</td><td>1.69</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.62</td><td>113</td><td>0.5</td><td>1.5</td><td>411</td><td>478</td></tr><tr><td>10DX261-29</td><td>Qz1</td><td>11.5</td><td>96.5</td><td>84.2</td><td>25.8</td><td>&lt;74.43</td><td>34.3</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>1.12</td><td>0.166</td><td>10.4</td><td>0.070<br>0</td><td>0.292</td><td>v.d.</td><td>0.62</td><td>111</td><td>0.5</td><td>1.5</td><td>447</td><td>520</td></tr><tr><td>10DX261-28</td><td>Qz1</td><td>10.2</td><td>51.2</td><td>104</td><td>36.8</td><td>&lt;89.38</td><td>22.3</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.793</td><td>1.40</td><td>0.430</td><td>0.844</td><td>0.188</td><td>0.914</td><td>0.731</td><td>0.62</td><td>137</td><td>0.5</td><td>1.5</td><td>420</td><td>489</td></tr><tr><td>10DX261-34</td><td>Qz1</td><td>12.7</td><td>&lt;2.5<br>8</td><td>120</td><td>23.4</td><td>89.0</td><td>21.7</td><td>0.226</td><td>v.d.</td><td>v.d.</td><td>1.22</td><td>0.348</td><td>1.29</td><td>0.390</td><td>0.180</td><td>0.087<br>0</td><td>0.189</td><td>0.36</td><td>0.62</td><td>158</td><td>0.5</td><td>1.5</td><td>418</td><td>487</td></tr><tr><td>12DXF05-5</td><td>Qz2<br>a</td><td>13.9</td><td>16.5</td><td>75.7</td><td>&lt;6.89</td><td>204</td><td>152</td><td>1.43</td><td>7.93</td><td>0.730</td><td>&lt;1.68</td><td>0.155</td><td>1.09</td><td>0.390</td><td>0.832</td><td>&lt;0.09<br>8</td><td>&lt;0.09<br>0</td><td>0.296</td><td>0.52</td><td>146</td><td>0.5</td><td>1.5</td><td>543</td><td>635</td></tr><tr><td>12DXF05-6</td><td>Qz2<br>a</td><td>14.8</td><td>25.5</td><td>59.2</td><td>&lt;3.92</td><td>&lt;75.23</td><td>56.9</td><td>1.32</td><td>7.42</td><td>0.202</td><td>0.550</td><td>0.171</td><td>1.10</td><td>&lt;0.18<br>8</td><td>1.41</td><td>0.057<br>0</td><td>&lt;0.05<br>7</td><td>0.491</td><td>0.52</td><td>114</td><td>0.5</td><td>1.5</td><td>479</td><td>559</td></tr><tr><td>12DXF05-7</td><td>Qz2<br>a</td><td>15.9</td><td>v.d.</td><td>207</td><td>108</td><td>215</td><td>193</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.179</td><td>0.64<br>4</td><td>0.920</td><td>1.46</td><td>&lt;0.07<br>2</td><td>0.304</td><td>v.d.</td><td>0.52</td><td>399</td><td>0.5</td><td>1.5</td><td>558</td><td>653</td></tr><tr><td>12DXF05-8</td><td>Qz2<br>a</td><td>15.4</td><td>v.d.</td><td>50.3</td><td>29.4</td><td>&lt;67.91</td><td>165</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.045</td><td>0.81</td><td>0.240</td><td>v.d.</td><td>&lt;0.05<br>4</td><td>0.09</td><td>v.d.</td><td>0.52</td><td>96.8</td><td>0.5</td><td>1.5</td><td>548</td><td>641</td></tr><tr><td>12DXF05-9</td><td>Qz2<br>a</td><td>13.9</td><td>&lt;3.8<br>3</td><td>56.7</td><td>&lt;6.52</td><td>&lt;127.1<br>5</td><td>167</td><td>&lt;0.070</td><td>2.39</td><td>&lt;0.25</td><td>&lt;0.99</td><td>0.133</td><td>0.81</td><td>&lt;0.35</td><td>0.136</td><td>0.219</td><td>&lt;0.07<br>5</td><td>0.979</td><td>0.52</td><td>109</td><td>0.5</td><td>1.5</td><td>549</td><td>643</td></tr><tr><td>12DXF05-10</td><td>Qz2<br>a</td><td>12.8</td><td>v.d.</td><td>53.5</td><td>66.0</td><td>101</td><td>90.6</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.114</td><td>0.75<br>7</td><td>0.233</td><td>v.d.</td><td>&lt;0.04<br>6</td><td>&lt;0.03<br>6</td><td>v.d.</td><td>0.52</td><td>103</td><td>0.5</td><td>1.5</td><td>510</td><td>595</td></tr><tr><td>12DXF05-11</td><td>Qz2<br>a</td><td>13.1</td><td>83.8</td><td>57.9</td><td>7.30</td><td>&lt;72.94</td><td>174</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.195</td><td>1.04</td><td>&lt;0.17<br>1</td><td>1.48</td><td>&lt;0.05<br>8</td><td>&lt;0.05<br>2</td><td>0.939</td><td>0.52</td><td>111</td><td>0.5</td><td>1.5</td><td>552</td><td>645</td></tr><tr><td>12DXF05-12</td><td>Qz2<br>a</td><td>23.3</td><td>71.7</td><td>225</td><td>110</td><td>105.9</td><td>97.6</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.114</td><td>0.87<br>1</td><td>&lt;0.20</td><td>0.349</td><td>0.228</td><td>0.042</td><td>1.29</td><td>0.52</td><td>433</td><td>0.5</td><td>1.5</td><td>515</td><td>601</td></tr><tr><td>12DXF05-13</td><td>Qz2<br>a</td><td>27.2</td><td>9.92</td><td>313</td><td>43.5</td><td>&lt;70.04</td><td>164</td><td>0.657</td><td>v.d.</td><td>&lt;0.13<br>0</td><td>1.25</td><td>0.0620</td><td>0.91<br>1</td><td>&lt;0.14<br>7</td><td>0.369</td><td>0.087</td><td>&lt;0.04<br>5</td><td>0.161</td><td>0.52</td><td>602</td><td>0.5</td><td>1.5</td><td>548</td><td>641</td></tr><tr><td>12DXF05-14</td><td>Qz2<br>a</td><td>17.4</td><td>v.d.</td><td>v.d.</td><td>133</td><td>&lt;84.66</td><td>130</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.0520</td><td>0.65<br>1</td><td>0.306</td><td>v.d.</td><td>&lt;0.06<br>9</td><td>0.057</td><td>v.d.</td><td>0.52</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>533</td><td>623</td></tr><tr><td>12DXF05-15</td><td>Qz2<br>a</td><td>27.5</td><td>49.8</td><td>218</td><td>62.5</td><td>&lt;50.53</td><td>157</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.0490</td><td>0.71<br>9</td><td>&lt;0.09<br>3</td><td>0.233</td><td>0.072</td><td>&lt;0.02<br>4</td><td>0.753</td><td>0.52</td><td>420</td><td>0.5</td><td>1.5</td><td>545</td><td>638</td></tr></table>
<table><tr><td>12DXF05-16</td><td>Qz2 a</td><td>14.0</td><td>124</td><td>56.8</td><td>46.8</td><td>&lt;61.76</td><td>110</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.0810</td><td>1.08</td><td>0.276</td><td>0.154</td><td>0.095</td><td>&lt;0.03 7</td><td>v.d.</td><td>0.52</td><td>109</td><td>0.5</td><td>1.5</td><td>522</td><td>610</td></tr><tr><td>12DXF05-19</td><td>Qz2 a</td><td>14.1</td><td>v.d.</td><td>v.d.</td><td>73.5</td><td>&lt;59.93</td><td>142</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.0440</td><td>1.01</td><td>0.406</td><td>v.d.</td><td>0.210</td><td>0.091</td><td>v.d.</td><td>0.52</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>539</td><td>630</td></tr><tr><td>12DXF05-26</td><td>Qz2 a</td><td>22.3</td><td>55.5</td><td>224</td><td>96.3</td><td>95.32</td><td>180</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.0850</td><td>1.03</td><td>&lt;0.19 4</td><td>v.d.</td><td>0.048</td><td>&lt;0.04 0</td><td>0</td><td>0.809</td><td>0.52</td><td>430</td><td>0.5</td><td>1.5</td><td>554</td><td>648</td></tr><tr><td>12DXF05-27</td><td>Qz2 a</td><td>11.2</td><td>v.d.</td><td>54.0</td><td>28.3</td><td>&lt;57.03</td><td>109</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.0188</td><td>0.89 4</td><td>1.06</td><td>0.513</td><td>&lt;0.04 8</td><td>0.085</td><td>v.d.</td><td>0.52</td><td>104</td><td>0.5</td><td>1.5</td><td>522</td><td>610</td></tr><tr><td>12DXF05-28</td><td>Qz2 a</td><td>13.5</td><td>80.2</td><td>67.0</td><td>13.2</td><td>&lt;67.38</td><td>159</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>&lt;0.010 4</td><td>0.80 6</td><td>&lt;0.20 7</td><td>0.297</td><td>0.065 0</td><td>0.084</td><td>v.d.</td><td>0.52</td><td>129</td><td>0.5</td><td>1.5</td><td>546</td><td>639</td></tr><tr><td>12DXF05-29</td><td>Qz2 a</td><td>11.4</td><td>45.7</td><td>70.0</td><td>14.2</td><td>&lt;79.92</td><td>152</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.100</td><td>1.21 4</td><td>0.270</td><td>0.926</td><td>0.078 0</td><td>&lt;0.04 6</td><td>v.d.</td><td>0.52</td><td>135</td><td>0.5</td><td>1.5</td><td>543</td><td>635</td></tr><tr><td>10DX140-50</td><td>Qz2 a</td><td>11.7</td><td>30.2</td><td>106</td><td>16.3</td><td>114</td><td>101</td><td>0.441</td><td>v.d.</td><td>0.990</td><td>0.560</td><td>0.0810</td><td>1.32</td><td>0.360</td><td>1.14</td><td>0.139</td><td>0.625</td><td>0.472</td><td>0.56</td><td>189</td><td>0.5</td><td>1.5</td><td>517</td><td>604</td></tr><tr><td>12DX500-1</td><td>Qz2 a</td><td>25.8</td><td>10.8</td><td>127</td><td>18.5</td><td>83.0</td><td>101</td><td>0.568</td><td>v.d.</td><td>0.305</td><td>&lt;0.33</td><td>0.167</td><td>0.72 0</td><td>0.450</td><td>0.169</td><td>0.058 0</td><td>0.046</td><td>0.262</td><td>0.56</td><td>226</td><td>0.5</td><td>1.5</td><td>517</td><td>604</td></tr><tr><td>12DX500-2</td><td>Qz2 a</td><td>31.2</td><td>13.5</td><td>126</td><td>14.7</td><td>v.d.</td><td>117</td><td>0.433</td><td>v.d.</td><td>&lt;0.12 9</td><td>&lt;0.37</td><td>0.0117</td><td>1.18</td><td>&lt;0.14 1</td><td>v.d.</td><td>0.053 0</td><td>0.187</td><td>0.654</td><td>0.56</td><td>226</td><td>0.5</td><td>1.5</td><td>526</td><td>615</td></tr><tr><td>12DX500-3</td><td>Qz2 a</td><td>21.5</td><td>46.6</td><td>108</td><td>29.0</td><td>329</td><td>101</td><td>0.800</td><td>v.d.</td><td>0.252</td><td>&lt;0.30</td><td>0.114</td><td>0.80 6</td><td>0.194</td><td>1.10</td><td>0.119</td><td>0.152</td><td>0.465</td><td>0.56</td><td>193</td><td>0.5</td><td>1.5</td><td>517</td><td>604</td></tr><tr><td>12DX500-4</td><td>Qz2 a</td><td>27.0</td><td>18.0</td><td>106</td><td>13.5</td><td>&lt;89.59</td><td>201</td><td>0.410</td><td>v.d.</td><td>0.400</td><td>&lt;1.28</td><td>0.0530</td><td>0.97 0</td><td>0.810</td><td>4.10</td><td>0.118</td><td>0.179</td><td>0.745</td><td>0.56</td><td>190</td><td>0.5</td><td>1.5</td><td>560</td><td>656</td></tr><tr><td>12DX500-5</td><td>Qz2 a</td><td>26.0</td><td>13.6</td><td>97.2</td><td>&lt;4.73</td><td>270</td><td>121</td><td>0.178</td><td>3.99</td><td>&lt;0.18 6</td><td>&lt;0.00</td><td>&lt;0.016 2</td><td>0.84 0</td><td>&lt;0.23</td><td>0.569</td><td>0.141</td><td>&lt;0.05 3</td><td>0.119</td><td>0.56</td><td>174</td><td>0.5</td><td>1.5</td><td>529</td><td>618</td></tr><tr><td>12DX500-6</td><td>Qz2 a</td><td>29.7</td><td>37.0</td><td>146</td><td>42.6</td><td>v.d.</td><td>123</td><td>v.d.</td><td>v.d.</td><td>1.45</td><td>2.33</td><td>0.236</td><td>0.79 5</td><td>&lt;0.24</td><td>v.d.</td><td>0.191</td><td>0.119</td><td>0.81</td><td>0.56</td><td>260</td><td>0.5</td><td>1.5</td><td>530</td><td>619</td></tr><tr><td>12DX500-7</td><td>Qz2 a</td><td>30.9</td><td>49.6</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>227</td><td>v.d.</td><td>v.d.</td><td>0.448</td><td>1.64</td><td>0.206</td><td>0.92 5</td><td>0.690</td><td>v.d.</td><td>0.042</td><td>0.079</td><td>0.415</td><td>0.56</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>567</td><td>664</td></tr><tr><td>12DX500-8</td><td>Qz2 a</td><td>28.0</td><td>13.2</td><td>86.7</td><td>10.7</td><td>47.0</td><td>147</td><td>0.251</td><td>v.d.</td><td>0.392</td><td>0.370</td><td>0.121</td><td>0.96 4</td><td>&lt;0.13 1</td><td>0.165</td><td>0.079</td><td>0.089</td><td>0.096</td><td>0.56</td><td>155</td><td>0.5</td><td>1.5</td><td>541</td><td>633</td></tr><tr><td>10DX172-12</td><td>Qz2 a</td><td>9.73</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>112</td><td>10.4</td><td>v.d.</td><td>31.6</td><td>3.52</td><td>0.454</td><td>0.90 8</td><td>1.96</td><td>v.d.</td><td>0.187</td><td>0.383</td><td>0.744</td><td>0.51</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>524</td><td>612</td></tr><tr><td>10DX172-20</td><td>Qz2 a</td><td>14.3</td><td>75.3</td><td>74.5</td><td>19.9</td><td>120</td><td>108</td><td>0.389</td><td>2.55</td><td>0.82</td><td>1</td><td>0.0830</td><td>0.69 4</td><td>0.280</td><td>0.241</td><td>0.068</td><td>0.093</td><td>0.243</td><td>0.51</td><td>146</td><td>0.5</td><td>1.5</td><td>521</td><td>609</td></tr><tr><td>10DX172-21</td><td>Qz2 a</td><td>15.6</td><td>19.5</td><td>64.4</td><td>&lt;4.82</td><td>&lt;93.21</td><td>91.7</td><td>0.297</td><td>4.09</td><td>0.38</td><td>&lt;1.08</td><td>0.0740</td><td>0.76 0</td><td>0.420</td><td>v.d.</td><td>&lt;0.06 7</td><td>&lt;0.06 4</td><td>0.113</td><td>0.51</td><td>126</td><td>0.5</td><td>1.5</td><td>511</td><td>596</td></tr></table>
<table><tr><td>12DXF05-16</td><td>Qz2 a</td><td>14.0</td><td>124</td><td>56.8</td><td>46.8</td><td>&lt;61.76</td><td>110</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.0810</td><td>1.08</td><td>0.276</td><td>0.154</td><td>0.095</td><td>&lt;0.03 7</td><td>v.d.</td><td>0.52</td><td>109</td><td>0.5</td><td>1.5</td><td>522</td><td>610</td></tr><tr><td>12DXF05-19</td><td>Qz2 a</td><td>14.1</td><td>v.d.</td><td>v.d.</td><td>73.5</td><td>&lt;59.93</td><td>142</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.0440</td><td>1.01</td><td>0.406</td><td>v.d.</td><td>0.210</td><td>0.091</td><td>v.d.</td><td>0.52</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>539</td><td>630</td></tr><tr><td>12DXF05-26</td><td>Qz2 a</td><td>22.3</td><td>55.5</td><td>224</td><td>96.3</td><td>95.32</td><td>180</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.0850</td><td>1.03</td><td>&lt;0.19 4</td><td>v.d.</td><td>0.048</td><td>&lt;0.04 0</td><td>0.809</td><td>0.52</td><td>430</td><td>0.5</td><td>1.5</td><td>554</td><td>648</td></tr><tr><td>12DXF05-27</td><td>Qz2 a</td><td>11.2</td><td>v.d.</td><td>54.0</td><td>28.3</td><td>&lt;57.03</td><td>109</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.0188</td><td>0.89 4</td><td>1.06</td><td>0.513</td><td>&lt;0.04 8</td><td>0.085</td><td>v.d.</td><td>0.52</td><td>104</td><td>0.5</td><td>1.5</td><td>522</td><td>610</td></tr><tr><td>12DXF05-28</td><td>Qz2 a</td><td>13.5</td><td>80.2</td><td>67.0</td><td>13.2</td><td>&lt;67.38</td><td>159</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>&lt;0.010 4</td><td>0.80 6</td><td>&lt;0.20 7</td><td>0.297</td><td>0.065 0</td><td>0.084</td><td>v.d.</td><td>0.52</td><td>129</td><td>0.5</td><td>1.5</td><td>546</td><td>639</td></tr><tr><td>12DXF05-29</td><td>Qz2 a</td><td>11.4</td><td>45.7</td><td>70.0</td><td>14.2</td><td>&lt;79.92</td><td>152</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.100</td><td>1.21 4</td><td>0.270</td><td>0.926</td><td>0.078 0</td><td>&lt;0.04 6</td><td>v.d.</td><td>0.52</td><td>135</td><td>0.5</td><td>1.5</td><td>543</td><td>635</td></tr><tr><td>10DX140-50</td><td>Qz2 a</td><td>11.7</td><td>30.2</td><td>106</td><td>16.3</td><td>114</td><td>101</td><td>0.441</td><td>v.d.</td><td>0.990</td><td>0.560</td><td>0.0810</td><td>1.32</td><td>0.360</td><td>1.14</td><td>0.139</td><td>0.625</td><td>0.472</td><td>0.56</td><td>189</td><td>0.5</td><td>1.5</td><td>517</td><td>604</td></tr><tr><td>12DX500-1</td><td>Qz2 a</td><td>25.8</td><td>10.8</td><td>127</td><td>18.5</td><td>83.0</td><td>101</td><td>0.568</td><td>v.d.</td><td>0.305</td><td>&lt;0.33</td><td>0.167</td><td>0.72 0</td><td>0.450</td><td>0.169</td><td>0.058 0</td><td>0.046</td><td>0.262</td><td>0.56</td><td>226</td><td>0.5</td><td>1.5</td><td>517</td><td>604</td></tr><tr><td>12DX500-2</td><td>Qz2 a</td><td>31.2</td><td>13.5</td><td>126</td><td>14.7</td><td>v.d.</td><td>117</td><td>0.433</td><td>v.d.</td><td>&lt;0.12 9</td><td>&lt;0.37</td><td>0.0117</td><td>1.18</td><td>&lt;0.14 1</td><td>v.d.</td><td>0.053 0</td><td>0.187</td><td>0.654</td><td>0.56</td><td>226</td><td>0.5</td><td>1.5</td><td>526</td><td>615</td></tr><tr><td>12DX500-3</td><td>Qz2 a</td><td>21.5</td><td>46.6</td><td>108</td><td>29.0</td><td>329</td><td>101</td><td>0.800</td><td>v.d.</td><td>0.252</td><td>&lt;0.30</td><td>0.114</td><td>0.80 6</td><td>0.194</td><td>1.10</td><td>0.119</td><td>0.152</td><td>0.465</td><td>0.56</td><td>193</td><td>0.5</td><td>1.5</td><td>517</td><td>604</td></tr><tr><td>12DX500-4</td><td>Qz2 a</td><td>27.0</td><td>18.0</td><td>106</td><td>13.5</td><td>&lt;89.59</td><td>201</td><td>0.410</td><td>v.d.</td><td>0.400</td><td>&lt;1.28</td><td>0.0530</td><td>0.97 0</td><td>0.810</td><td>4.10</td><td>0.118</td><td>0.179</td><td>0.745</td><td>0.56</td><td>190</td><td>0.5</td><td>1.5</td><td>560</td><td>656</td></tr><tr><td>12DX500-5</td><td>Qz2 a</td><td>26.0</td><td>13.6</td><td>97.2</td><td>&lt;4.73</td><td>270</td><td>121</td><td>0.178</td><td>3.99</td><td>&lt;0.18 6</td><td>&lt;0.00</td><td>&lt;0.016 2</td><td>0.84 0</td><td>&lt;0.23</td><td>0.569</td><td>0.141</td><td>&lt;0.05 3</td><td>0.119</td><td>0.56</td><td>174</td><td>0.5</td><td>1.5</td><td>529</td><td>618</td></tr><tr><td>12DX500-6</td><td>Qz2 a</td><td>29.7</td><td>37.0</td><td>146</td><td>42.6</td><td>v.d.</td><td>123</td><td>v.d.</td><td>v.d.</td><td>1.45</td><td>2.33</td><td>0.236</td><td>0.79 5</td><td>&lt;0.24</td><td>v.d.</td><td>0.191</td><td>0.119</td><td>0.81</td><td>0.56</td><td>260</td><td>0.5</td><td>1.5</td><td>530</td><td>619</td></tr><tr><td>12DX500-7</td><td>Qz2 a</td><td>30.9</td><td>49.6</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>227</td><td>v.d.</td><td>v.d.</td><td>0.448</td><td>1.64</td><td>0.206</td><td>0.92 5</td><td>0.690</td><td>v.d.</td><td>0.042</td><td>0.079</td><td>0.415</td><td>0.56</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>567</td><td>664</td></tr><tr><td>12DX500-8</td><td>Qz2 a</td><td>28.0</td><td>13.2</td><td>86.7</td><td>10.7</td><td>47.0</td><td>147</td><td>0.251</td><td>v.d.</td><td>0.392</td><td>0.370</td><td>0.121</td><td>0.96 4</td><td>&lt;0.13 1</td><td>0.165</td><td>0.079</td><td>0.089</td><td>0.096</td><td>0.56</td><td>155</td><td>0.5</td><td>1.5</td><td>541</td><td>633</td></tr><tr><td>10DX172-12</td><td>Qz2 a</td><td>9.73</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>112</td><td>10.4</td><td>v.d.</td><td>31.6</td><td>3.52</td><td>0.454</td><td>0.90 8</td><td>1.96</td><td>v.d.</td><td>0.187</td><td>0.383</td><td>0.744</td><td>0.51</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>524</td><td>612</td></tr><tr><td>10DX172-20</td><td>Qz2 a</td><td>14.3</td><td>75.3</td><td>74.5</td><td>19.9</td><td>120</td><td>108</td><td>0.389</td><td>2.55</td><td>0.82</td><td>1</td><td>0.0830</td><td>0.69 4</td><td>0.280</td><td>0.241</td><td>0.068</td><td>0.093</td><td>0.243</td><td>0.51</td><td>146</td><td>0.5</td><td>1.5</td><td>521</td><td>609</td></tr><tr><td>10DX172-21</td><td>Qz2 a</td><td>15.6</td><td>19.5</td><td>64.4</td><td>&lt;4.82</td><td>&lt;93.21</td><td>91.7</td><td>0.297</td><td>4.09</td><td>0.38</td><td>&lt;1.08</td><td>0.0740</td><td>0.76 0</td><td>0.420</td><td>v.d.</td><td>&lt;0.06 7</td><td>&lt;0.06 4</td><td>0.113</td><td>0.51</td><td>126</td><td>0.5</td><td>1.5</td><td>511</td><td>596</td></tr></table>
<table><tr><td>10DX172-22</td><td>Qz2 a</td><td>15.7 50.2 78.8 10.8</td><td>&lt;67.38 118 0.127</td><td>2.24 0.215 &lt;1.06 0.0241</td><td>0.79 0 0.580 0.483 0.046</td><td>&lt;0.04 5 &lt;0.026</td><td>0.51</td><td>154</td><td>0.5</td><td>1.5</td><td>527</td><td>616</td></tr><tr><td>10DX328-1</td><td>Qz2 a</td><td>17.7 v.d. 116 v.d.</td><td>v.d. 85.3 3.58</td><td>v.d. 1.30 &lt;0.88 0.036</td><td>0.54 0 &lt;0.26 v.d.</td><td>&lt;0.04 5 0.076 0.946</td><td>0.76</td><td>153</td><td>0.5</td><td>1.5</td><td>506</td><td>591</td></tr><tr><td>10DX328-2</td><td>Qz2 a</td><td>17.2 6.92 121 v.d.</td><td>&lt;88.55 100 0.423</td><td>7.76 0.800 &lt;1.18</td><td>&lt;0.020 9 1.21 0.320 0.569</td><td>&lt;0.06 3 4 &lt;0.06 4 0.049</td><td>0.76</td><td>159</td><td>0.5</td><td>1.5</td><td>517</td><td>603</td></tr><tr><td>10DX328-3</td><td>Qz2 a</td><td>21.5 v.d. 159 v.d.</td><td>79.83 87.6 0.133</td><td>4.90 &lt;0.23 8 &lt;0.64 0.0519</td><td>0.85 9 &lt;0.22 0.211 0.074 0.143</td><td>0.073</td><td>0.76</td><td>209</td><td>0.5</td><td>1.5</td><td>508</td><td>593</td></tr><tr><td>10DX328-5</td><td>Qz2 a</td><td>13.5 62.4 87.7 8.34</td><td>&lt;82.29 68.2 v.d.</td><td>v.d. v.d. 0.99 0.305</td><td>1.39 0.340 0.139 0.187 0.078</td><td>0.839</td><td>0.76</td><td>115</td><td>0.5</td><td>1.5</td><td>491</td><td>573</td></tr><tr><td>10DX328-6</td><td>Qz2 a</td><td>17.1 v.d. 90.2 17.0</td><td>78.9 96.8 v.d.</td><td>v.d. v.d. 1.66 0.008 4</td><td>1.59 &lt;0.22 0.099 0 0.088 0</td><td>&lt;0.03 0 v.d.</td><td>0.76</td><td>119</td><td>0.5</td><td>1.5</td><td>514</td><td>601</td></tr><tr><td>10DX328-7</td><td>Qz2 a</td><td>15.2 70.4 97.3 16.8</td><td>&lt;49.84 90.1 v.d.</td><td>v.d. v.d. 1.56 &lt;0.016</td><td>1.19 0.270 0.193 0.112</td><td>0.046 0 v.d.</td><td>0.76</td><td>128</td><td>0.5</td><td>1.5</td><td>510</td><td>595</td></tr><tr><td>10DX328-10</td><td>Qz2 a</td><td>15.3 v.d. 133 43.1</td><td>85.8 79.0 v.d.</td><td>v.d. v.d. 4.63 0.0950</td><td>1.23 0.730 0.551 0.155</td><td>0.093 0 v.d.</td><td>0.76</td><td>176</td><td>0.5</td><td>1.5</td><td>501</td><td>585</td></tr><tr><td>10DX328-11</td><td>Qz2 a</td><td>16.5 9.55 v.d. v.d.</td><td>v.d. 96.8 v.d.</td><td>v.d. v.d. v.d. 0.0430</td><td>1.1 0.580 v.d. 0.09</td><td>&lt;0.08 5 v.d.</td><td>0.76</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>514</td><td>601</td></tr><tr><td>10DX22-4</td><td>Qz2 a</td><td>15.3 10.8 78.9 &lt;3.48</td><td>&lt;65.83 130 0.314</td><td>4.10 0.927 0.390 0.107</td><td>0.66 1 0 &lt;0.16 v.d.</td><td>&lt;0.06 5 0.108 0.105</td><td>0.55</td><td>143</td><td>0.5</td><td>1.5</td><td>533</td><td>624</td></tr><tr><td>10DX22-5</td><td>Qz2 a</td><td>15.9 35.2 v.d. 185</td><td>210 160 1.31</td><td>v.d. 0.214 1.06 0.125</td><td>0.85 4 0.306 0.582 0.186 0.161</td><td>0.253</td><td>0.55</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>546</td><td>639</td></tr><tr><td>10DX22-7</td><td>Qz2 a</td><td>15.8 27.8 v.d. 273</td><td>75.6 143 0.947</td><td>v.d. 0.291 &lt;0.46 0.133</td><td>0.93 3 9 &lt;0.18 0.565 0.108 0.177</td><td>0.17</td><td>0.55</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>539</td><td>630</td></tr><tr><td>10DX22-20</td><td>Qz2 a</td><td>17.6 3.34 76.4 4.1</td><td>&lt;49.37 129 0.156</td><td>4.67 1.47 &lt;0.58 0.160</td><td>1.06 0.224 0.982 0.093</td><td>0.048 0 0.184</td><td>0.55</td><td>139</td><td>0.5</td><td>1.5</td><td>533</td><td>623</td></tr><tr><td>10DX168-2</td><td>Qz2 b</td><td>13.1 7 55.6 &lt;5.46</td><td>100 57.2 &lt;0.064 1.41</td><td>&lt;0.19 2 &lt;0.83 0.229 0.45 0.710</td><td>0.011 8 0.209 4</td><td>&lt;0.05 4 0.142</td><td>0.58</td><td>95.9</td><td>0.5</td><td>1.5</td><td>480</td><td>559</td></tr><tr><td>10DX168-4</td><td>Qz2 b</td><td>9.34 10.8 50.5 &lt;7.86</td><td>&lt;148.2 9 47.9 0.509</td><td>3.93 0.900 &lt;1.14 0.028</td><td>0.76 &lt;0.48 0.755</td><td>&lt;0.09 9 0.10 5 0.069</td><td>0.58</td><td>87.1</td><td>0.5</td><td>1.5</td><td>468</td><td>546</td></tr><tr><td>10DX168-5</td><td>Qz2 b</td><td>12.0 4 47.9 &lt;6.26</td><td>&lt;113.2 0 62.6 &lt;0.069</td><td>1.3 0.720 1.17 0.310</td><td>1.25 &lt;0.34 0.007 3 1 7</td><td>&lt;0.08 1 7 &lt;0.08 7 0.082</td><td>0.58</td><td>82.6</td><td>0.5</td><td>1.5</td><td>486</td><td>566</td></tr><tr><td>10DX168-7</td><td>Qz2 b</td><td>7.93 34.7 62.4 &lt;5.49</td><td>&lt;102.7 8 53.6 v.d.</td><td>v.d. v.d. &lt;0.75 0.0267 1.01</td><td>&lt;0.15 7 0.029 5</td><td>0.072 0.239 0.385</td><td>0.58</td><td>108</td><td>0.5</td><td>1.5</td><td>476</td><td>554</td></tr><tr><td>10DX168-8</td><td>Qz2 b</td><td>11.7 18.0 56.2 3.87</td><td>&lt;52.12 62.2 0.279</td><td>2.35 0.446 &lt;0.37 0.0310 0.97 0.165</td><td>0.026 9 0.134 0.152 0.234</td><td>0.234</td><td>0.58</td><td>96.9</td><td>0.5</td><td>1.5</td><td>485</td><td>566</td></tr></table>
<table><tr><td>10DX172-22</td><td>Qz2 a</td><td>15.7 50.2 78.8 10.8</td><td>&lt;67.38 118 0.127</td><td>2.24 0.215 &lt;1.06 0.0241</td><td>0.79 0 0.580 0.483 0.046</td><td>&lt;0.04 5 &lt;0.026</td><td>0.51</td><td>154</td><td>0.5</td><td>1.5</td><td>527</td><td>616</td></tr><tr><td>10DX328-1</td><td>Qz2 a</td><td>17.7 v.d. 116 v.d.</td><td>v.d. 85.3 3.58</td><td>v.d. 1.30 &lt;0.88 0.036</td><td>0.54 0 &lt;0.26 v.d.</td><td>&lt;0.04 5 0.076</td><td>0.946</td><td>0.76</td><td>153</td><td>0.5</td><td>1.5</td><td>506</td><td>591</td></tr><tr><td>10DX328-2</td><td>Qz2 a</td><td>17.2 6.92 121 v.d.</td><td>&lt;88.55 100 0.423</td><td>7.76 0.800 &lt;1.18</td><td>&lt;0.020 9 1.21 0.320 0.569</td><td>&lt;0.06 3 0.049</td><td>0.049</td><td>0.76</td><td>159</td><td>0.5</td><td>1.5</td><td>517</td><td>603</td></tr><tr><td>10DX328-3</td><td>Qz2 a</td><td>21.5 v.d. 159 v.d.</td><td>79.83 87.6 0.133</td><td>4.90 &lt;0.23 8 &lt;0.64 0.0519</td><td>0.85 9 &lt;0.22 0.211 0.074</td><td>0.143 0.073</td><td>0.073</td><td>0.76</td><td>209</td><td>0.5</td><td>1.5</td><td>508</td><td>593</td></tr><tr><td>10DX328-5</td><td>Qz2 a</td><td>13.5 62.4 87.7 8.34</td><td>&lt;82.29 68.2 v.d.</td><td>v.d. v.d. 0.99 0.305</td><td>1.39 0.340 0.139 0.187</td><td>0.078 0.839</td><td>0.839</td><td>0.76</td><td>115</td><td>0.5</td><td>1.5</td><td>491</td><td>573</td></tr><tr><td>10DX328-6</td><td>Qz2 a</td><td>17.1 v.d. 90.2 17.0</td><td>78.9 96.8 v.d.</td><td>v.d. v.d. 1.66 0.008 4</td><td>1.59 &lt;0.22 0.099 0 0.088</td><td>&lt;0.03 0 v.d.</td><td>0.76</td><td>119</td><td>0.5</td><td>1.5</td><td>514</td><td>601</td></tr><tr><td>10DX328-7</td><td>Qz2 a</td><td>15.2 70.4 97.3 16.8</td><td>&lt;49.84 90.1 v.d.</td><td>v.d. v.d. 1.56 &lt;0.016</td><td>1.19 0.270 0.193 0.112</td><td>0.046 0 v.d.</td><td>0.76</td><td>128</td><td>0.5</td><td>1.5</td><td>510</td><td>595</td></tr><tr><td>10DX328-10</td><td>Qz2 a</td><td>15.3 v.d. 133 43.1</td><td>85.8 79.0 v.d.</td><td>v.d. v.d. 4.63 0.0950</td><td>1.23 0.730 0.551 0.155</td><td>0.093 0 v.d.</td><td>0.76</td><td>176</td><td>0.5</td><td>1.5</td><td>501</td><td>585</td></tr><tr><td>10DX328-11</td><td>Qz2 a</td><td>16.5 9.55 v.d. v.d.</td><td>v.d. 96.8 v.d.</td><td>v.d. v.d. v.d. 0.0430</td><td>1.1 0.580 v.d. 0.09</td><td>&lt;0.08 5 v.d.</td><td>0.76</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>514</td><td>601</td></tr><tr><td>10DX22-4</td><td>Qz2 a</td><td>15.3 10.8 78.9 &lt;3.48</td><td>&lt;65.83 130 0.314</td><td>4.10 0.927 0.390 0.107</td><td>0.66 1 0 v.d. &lt;0.06 5</td><td>0.108 0.105</td><td>0.105</td><td>0.55</td><td>143</td><td>0.5</td><td>1.5</td><td>533</td><td>624</td></tr><tr><td>10DX22-5</td><td>Qz2 a</td><td>15.9 35.2 v.d. 185</td><td>210 160 1.31</td><td>v.d. 0.214 1.06 0.125</td><td>0.85 4 0.306 0.582 0.186</td><td>0.161 0.253</td><td>0.253</td><td>0.55</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>546</td><td>639</td></tr><tr><td>10DX22-7</td><td>Qz2 a</td><td>15.8 27.8 v.d. 273</td><td>75.6 143 0.947</td><td>v.d. 0.291 &lt;0.46 0.133</td><td>0.93 3 0.565 0.108 0.177</td><td>0.17 0.17</td><td>0.17</td><td>0.55</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>539</td><td>630</td></tr><tr><td>10DX22-20</td><td>Qz2 a</td><td>17.6 3.34 76.4 4.1</td><td>&lt;49.37 129 0.156</td><td>4.67 1.47 &lt;0.58 0.160</td><td>1.06 0.224 0.982 0.093</td><td>0.048 0 0.184</td><td>0.184</td><td>0.55</td><td>139</td><td>0.5</td><td>1.5</td><td>533</td><td>623</td></tr><tr><td>10DX168-2</td><td>Qz2 b</td><td>13.1 7 55.6 &lt;5.46</td><td>100 57.2 &lt;0.064 1.41</td><td>&lt;0.19 2 &lt;0.83 0.229 0.45</td><td>0.710 8 0.209 0.011 4</td><td>&lt;0.05 4 0.142</td><td>0.142</td><td>0.58</td><td>95.9</td><td>0.5</td><td>1.5</td><td>480</td><td>559</td></tr><tr><td>10DX168-4</td><td>Qz2 b</td><td>9.34 10.8 50.5 &lt;7.86</td><td>&lt;148.2 9 47.9 0.509</td><td>3.93 0.900 &lt;1.14 0.028</td><td>0.76 &lt;0.48 0.755</td><td>&lt;0.09 9 0.069</td><td>0.069</td><td>0.58</td><td>87.1</td><td>0.5</td><td>1.5</td><td>468</td><td>546</td></tr><tr><td>10DX168-5</td><td>Qz2 b</td><td>12.0 4 47.9 &lt;6.26</td><td>&lt;113.2 0 62.6 &lt;0.069</td><td>1.3 0.720 1.17 0.310</td><td>1.25 &lt;0.34 0.007 3 0.08 1 0.082</td><td>&lt;0.08 1 7</td><td>0.082</td><td>0.58</td><td>82.6</td><td>0.5</td><td>1.5</td><td>486</td><td>566</td></tr><tr><td>10DX168-7</td><td>Qz2 b</td><td>7.93 34.7 62.4 &lt;5.49</td><td>&lt;102.7 8 53.6 v.d.</td><td>v.d. v.d. &lt;0.75 0.0267 1.01</td><td>&lt;0.15 7 0.029 5</td><td>0.072 0.239 0.385</td><td>0.385</td><td>0.58</td><td>108</td><td>0.5</td><td>1.5</td><td>476</td><td>554</td></tr><tr><td>10DX168-8</td><td>Qz2 b</td><td>11.7 18.0 56.2 3.87</td><td>&lt;52.12 62.2 0.279</td><td>2.35 0.446 &lt;0.37 0.0310 0.97</td><td>0.165 9 0.134 0.152 0.234</td><td>0.234</td><td>0.234</td><td>0.58</td><td>96.9</td><td>0.5</td><td>1.5</td><td>485</td><td>566</td></tr></table>
<table><tr><td>10DX168-10</td><td>Qz2 b</td><td>9.88</td><td>26.9</td><td>56.5</td><td>&lt;3.90</td><td>150</td><td>64.7</td><td>0.494</td><td>1.47</td><td>0.920</td><td>0.44</td><td>0.0310</td><td>0.937</td><td>0.470</td><td>0.0389</td><td>0.136</td><td>0.427</td><td>0.179</td><td>0.58</td><td>97.3</td><td>0.5</td><td>1.5</td><td>488</td><td>569</td></tr><tr><td>10DX168-14</td><td>Qz2 b</td><td>10.9</td><td>47.4</td><td>61.2</td><td>7.44</td><td>&lt;93.37</td><td>61.4</td><td>0.461</td><td>2.81</td><td>0.640</td><td>&lt;0.84</td><td>0.0370</td><td>0.9</td><td>&lt;0.204</td><td>0.298</td><td>0.110</td><td>0.140</td><td>0.534</td><td>0.58</td><td>106</td><td>0.5</td><td>1.5</td><td>484</td><td>565</td></tr><tr><td>10DX168-16</td><td>Qz2 b</td><td>7.67</td><td>48.0</td><td>45.0</td><td>13.1</td><td>&lt;74.34</td><td>39.7</td><td>0.125</td><td>v.d.</td><td>v.d.</td><td>&lt;0.37</td><td>0.0590</td><td>1.22</td><td>0.362</td><td>0.227</td><td>0.058</td><td>0.0910</td><td>0.156</td><td>0.58</td><td>77.6</td><td>0.5</td><td>1.5</td><td>456</td><td>531</td></tr><tr><td>10DX168-26</td><td>Qz2 b</td><td>8.81</td><td>49.7</td><td>46.5</td><td>14.0</td><td>357</td><td>16.2</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>&lt;0.43</td><td>0.0270</td><td>1.54</td><td>0.540</td><td>v.d.</td><td>0.063</td><td>0.215</td><td>0.343</td><td>0.58</td><td>80.2</td><td>0.5</td><td>1.5</td><td>401</td><td>467</td></tr><tr><td>10DX168-29</td><td>Qz2 b</td><td>6.70</td><td>62.8</td><td>58.6</td><td>5.43</td><td>v.d.</td><td>49.2</td><td>1.32</td><td>v.d.</td><td>v.d.</td><td>&lt;0.37</td><td>0.0940</td><td>1.14</td><td>0.950</td><td>v.d.</td><td>0.047</td><td>0.257</td><td>0.253</td><td>0.58</td><td>101</td><td>0.5</td><td>1.5</td><td>470</td><td>548</td></tr><tr><td>10DX168-32</td><td>Qz2 b</td><td>10.8</td><td>68.9</td><td>87.0</td><td>20.3</td><td>82.2</td><td>61.0</td><td>0.146</td><td>5.20</td><td>v.d.</td><td>&lt;0.00</td><td>0.0211</td><td>0.831</td><td>v.d.</td><td>v.d.</td><td>0.032</td><td>0.130</td><td>0.089</td><td>0.58</td><td>150</td><td>0.5</td><td>1.5</td><td>484</td><td>564</td></tr><tr><td>10DX168-35</td><td>Qz2 b</td><td>8.42</td><td>57.7</td><td>v.d.</td><td>70.3</td><td>&lt;104.08</td><td>54.7</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.0550</td><td>0.880</td><td>1.14</td><td>0.143</td><td>0.234</td><td>0.788</td><td>v.d.</td><td>0.58</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>477</td><td>556</td></tr><tr><td>10DX168-36</td><td>Qz2 b</td><td>18.5</td><td>19.7</td><td>81.7</td><td>9.18</td><td>106</td><td>65.3</td><td>0.0980</td><td>2.35</td><td>v.d.</td><td>&lt;0.48</td><td>0.125</td><td>1.09</td><td>0.640</td><td>0.0960</td><td>&lt;0.072</td><td>0.224</td><td>0.751</td><td>0.58</td><td>141</td><td>0.5</td><td>1.5</td><td>488</td><td>570</td></tr><tr><td>10DX168-37</td><td>Qz2 b</td><td>15.1</td><td>57.2</td><td>95.5</td><td>9.5</td><td>&lt;62.55</td><td>72.9</td><td>0.120</td><td>4.80</td><td>v.d.</td><td>&lt;0.59</td><td>0.0910</td><td>0.868</td><td>0.231</td><td>0.122</td><td>0.18</td><td>0.305</td><td>0.182</td><td>0.58</td><td>165</td><td>0.5</td><td>1.5</td><td>496</td><td>578</td></tr><tr><td>10DX168-38</td><td>Qz2 b</td><td>25.3</td><td>&lt;3.13</td><td>77.1</td><td>&lt;5.46</td><td>124</td><td>68.7</td><td>&lt;0.051</td><td>1.60</td><td>&lt;0.21</td><td>&lt;0.00</td><td>0.843</td><td>1.41</td><td>0.590</td><td>0.0249</td><td>&lt;0.068</td><td>0.391</td><td>0.309</td><td>0.58</td><td>133</td><td>0.5</td><td>1.5</td><td>492</td><td>574</td></tr><tr><td>10DX168-39</td><td>Qz2 b</td><td>13.3</td><td>25.1</td><td>53.7</td><td>&lt;3.86</td><td>&lt;68.75</td><td>31.8</td><td>&lt;0.036</td><td>1.415</td><td>v.d.</td><td>&lt;0.52</td><td>0.222</td><td>1.38</td><td>1.18</td><td>0.0900</td><td>0.066</td><td>0.176</td><td>0.252</td><td>0.58</td><td>92.5</td><td>0.5</td><td>1.5</td><td>442</td><td>515</td></tr><tr><td>10DX168-40</td><td>Qz2 b</td><td>7.35</td><td>30.2</td><td>45.7</td><td>5.56</td><td>&lt;77.67</td><td>45.5</td><td>&lt;0.047</td><td>0.870</td><td>v.d.</td><td>&lt;0.89</td><td>0.0880</td><td>0.719</td><td>&lt;0.30</td><td>0.0698</td><td>&lt;0.061</td><td>0.317</td><td>0.066</td><td>0.58</td><td>78.8</td><td>0.5</td><td>1.5</td><td>465</td><td>542</td></tr><tr><td>DX168GY-01</td><td>Qz2 b</td><td>8.96</td><td>0.349</td><td>69.7</td><td>0.00</td><td>20.4</td><td>36.2</td><td>0.291</td><td>v.d.</td><td>0.000</td><td>0.261</td><td>0.010</td><td>0.949</td><td>0.267</td><td>0.002</td><td>0.228</td><td>0.016</td><td>0.005</td><td>v.d.</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>450</td><td>524</td></tr><tr><td>DX168GY-02</td><td>Qz2 b</td><td>8.59</td><td>v.d.</td><td>194</td><td>398</td><td>82.3</td><td>59.7</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>14.5</td><td>0.127</td><td>0.787</td><td>0.636</td><td>v.d.</td><td>0.454</td><td>0.064</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>483</td><td>563</td></tr><tr><td>DX168GY-03</td><td>Qz2 b</td><td>11.9</td><td>1.03</td><td>101</td><td>0.00</td><td>29.2</td><td>51.5</td><td>0.411</td><td>0.864</td><td>0.099</td><td>0.000</td><td>0.003</td><td>0.701</td><td>0.179</td><td>0.002</td><td>0.320</td><td>0.001</td><td>0.000</td><td>v.d.</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>473</td><td>551</td></tr><tr><td>DX168GY-05</td><td>Qz2 b</td><td>19.9</td><td>19.3</td><td>242</td><td>20.4</td><td>0.00</td><td>50.8</td><td>1.25</td><td>7.195</td><td>0.315</td><td>0.263</td><td>0.000</td><td>0.835</td><td>0.393</td><td>0.111</td><td>0.257</td><td>0.038</td><td>0.062</td><td>v.d.</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>472</td><td>550</td></tr><tr><td>DX168GY-06</td><td>Qz2 b</td><td>11.9</td><td>23.6</td><td>126</td><td>7.05</td><td>0.00</td><td>50.5</td><td>0.000</td><td>1.449</td><td>0.030</td><td>0.000</td><td>0.018</td><td>0.852</td><td>0.780</td><td>0.484</td><td>0.282</td><td>0.172</td><td>0.000</td><td>v.d.</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>472</td><td>550</td></tr><tr><td>DX168GY-07</td><td>Qz2 b</td><td>15.1</td><td>64.7</td><td>164</td><td>18.7</td><td>75.1</td><td>50.1</td><td>0.355</td><td>4.855</td><td>1.523</td><td>0.111</td><td>0.015</td><td>0.689</td><td>0.721</td><td>0.078</td><td>0.207</td><td>0.134</td><td>0.050</td><td>v.d.</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>471</td><td>549</td></tr></table>
<table><tr><td>10DX168-10</td><td>Qz2 b</td><td>9.88</td><td>26.9</td><td>56.5</td><td>&lt;3.90</td><td>150</td><td>64.7</td><td>0.494</td><td>1.47</td><td>0.920</td><td>0.44</td><td>0.0310</td><td>0.93 7</td><td>0.470</td><td>0.038 9</td><td>0.136</td><td>0.427</td><td>0.179</td><td>0.58</td><td>97.3</td><td>0.5</td><td>1.5</td><td>488</td><td>569</td></tr><tr><td>10DX168-14</td><td>Qz2 b</td><td>10.9</td><td>47.4</td><td>61.2</td><td>7.44</td><td>&lt;93.37</td><td>61.4</td><td>0.461</td><td>2.81</td><td>0.640</td><td>&lt;0.84</td><td>0.0370</td><td>0.9</td><td>&lt;0.20 4</td><td>0.298</td><td>0.110</td><td>0.140</td><td>0.534</td><td>0.58</td><td>106</td><td>0.5</td><td>1.5</td><td>484</td><td>565</td></tr><tr><td>10DX168-16</td><td>Qz2 b</td><td>7.67</td><td>48.0</td><td>45.0</td><td>13.1</td><td>&lt;74.34</td><td>39.7</td><td>0.125</td><td>v.d.</td><td>v.d.</td><td>&lt;0.37</td><td>0.0590</td><td>1.22</td><td>0.362</td><td>0.227</td><td>0.058</td><td>0.091 0</td><td>0.156</td><td>0.58</td><td>77.6</td><td>0.5</td><td>1.5</td><td>456</td><td>531</td></tr><tr><td>10DX168-26</td><td>Qz2 b</td><td>8.81</td><td>49.7</td><td>46.5</td><td>14.0</td><td>357</td><td>16.2</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>&lt;0.43</td><td>0.0270</td><td>1.54</td><td>0.540</td><td>v.d.</td><td>0.063</td><td>0.215</td><td>0.343</td><td>0.58</td><td>80.2</td><td>0.5</td><td>1.5</td><td>401</td><td>467</td></tr><tr><td>10DX168-29</td><td>Qz2 b</td><td>6.70</td><td>62.8</td><td>58.6</td><td>5.43</td><td>v.d.</td><td>49.2</td><td>1.32</td><td>v.d.</td><td>v.d.</td><td>&lt;0.37</td><td>0.0940</td><td>1.14</td><td>0.950</td><td>v.d.</td><td>0.047</td><td>0.257</td><td>0.253</td><td>0.58</td><td>101</td><td>0.5</td><td>1.5</td><td>470</td><td>548</td></tr><tr><td>10DX168-32</td><td>Qz2 b</td><td>10.8</td><td>68.9</td><td>87.0</td><td>20.3</td><td>82.2</td><td>61.0</td><td>0.146</td><td>5.20</td><td>v.d.</td><td>&lt;0.00</td><td>0.0211</td><td>0.83 1</td><td>v.d.</td><td>v.d.</td><td>0.032</td><td>0.130</td><td>0.089</td><td>0.58</td><td>150</td><td>0.5</td><td>1.5</td><td>484</td><td>564</td></tr><tr><td>10DX168-35</td><td>Qz2 b</td><td>8.42</td><td>57.7</td><td>v.d.</td><td>70.3</td><td>&lt;104.0 8</td><td>54.7</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.0550</td><td>0.88 0</td><td>1.14</td><td>0.143</td><td>0.234</td><td>0.788</td><td>v.d.</td><td>0.58</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>477</td><td>556</td></tr><tr><td>10DX168-36</td><td>Qz2 b</td><td>18.5</td><td>19.7</td><td>81.7</td><td>9.18</td><td>106</td><td>65.3</td><td>0.0980</td><td>2.35</td><td>v.d.</td><td>&lt;0.48</td><td>0.125</td><td>1.09</td><td>0.640</td><td>0.096 0</td><td>&lt;0.07 2</td><td>0.224</td><td>0.751</td><td>0.58</td><td>141</td><td>0.5</td><td>1.5</td><td>488</td><td>570</td></tr><tr><td>10DX168-37</td><td>Qz2 b</td><td>15.1</td><td>57.2</td><td>95.5</td><td>9.5</td><td>&lt;62.55</td><td>72.9</td><td>0.120</td><td>4.80</td><td>v.d.</td><td>&lt;0.59</td><td>0.0910</td><td>0.86 8</td><td>0.231</td><td>0.122</td><td>0.18</td><td>0.305</td><td>0.182</td><td>0.58</td><td>165</td><td>0.5</td><td>1.5</td><td>496</td><td>578</td></tr><tr><td>10DX168-38</td><td>Qz2 b</td><td>25.3</td><td>&lt;3.1 3</td><td>77.1</td><td>&lt;5.46</td><td>124</td><td>68.7</td><td>&lt;0.051</td><td>1.60</td><td>&lt;0.21</td><td>&lt;0.00</td><td>0.843</td><td>1.41</td><td>0.590</td><td>0.024 9</td><td>&lt;0.06 8</td><td>0.391</td><td>0.309</td><td>0.58</td><td>133</td><td>0.5</td><td>1.5</td><td>492</td><td>574</td></tr><tr><td>10DX168-39</td><td>Qz2 b</td><td>13.3</td><td>25.1</td><td>53.7</td><td>&lt;3.86</td><td>&lt;68.75</td><td>31.8</td><td>&lt;0.036</td><td>1.415</td><td>v.d.</td><td>&lt;0.52</td><td>0.222</td><td>1.38</td><td>1.18</td><td>0.090 0</td><td>0.066</td><td>0.176</td><td>0.252</td><td>0.58</td><td>92.5</td><td>0.5</td><td>1.5</td><td>442</td><td>515</td></tr><tr><td>10DX168-40</td><td>Qz2 b</td><td>7.35</td><td>30.2</td><td>45.7</td><td>5.56</td><td>&lt;77.67</td><td>45.5</td><td>&lt;0.047</td><td>0.870</td><td>v.d.</td><td>&lt;0.89</td><td>0.0880</td><td>0.71 9</td><td>&lt;0.30</td><td>0.069 8</td><td>&lt;0.06 1</td><td>0.317</td><td>0.066</td><td>0.58</td><td>78.8</td><td>0.5</td><td>1.5</td><td>465</td><td>542</td></tr><tr><td>DX168GY-01</td><td>Qz2 b</td><td>8.96</td><td>0.34 9</td><td>69.7</td><td>0.00</td><td>20.4</td><td>36.2</td><td>0.291</td><td>v.d.</td><td>0.000</td><td>0.261</td><td>0.010</td><td>0.94 9</td><td>0.267</td><td>0.002</td><td>0.228</td><td>0.016</td><td>0.005</td><td>v.d.</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>450</td><td>524</td></tr><tr><td>DX168GY-02</td><td>Qz2 b</td><td>8.59</td><td>v.d.</td><td>194</td><td>398</td><td>82.3</td><td>59.7</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>14.5</td><td>0.127</td><td>0.78 7</td><td>0.636</td><td>v.d.</td><td>0.454</td><td>0.064</td><td>v.d.</td><td>v.d.</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>483</td><td>563</td></tr><tr><td>DX168GY-03</td><td>Qz2 b</td><td>11.9</td><td>1.03</td><td>101</td><td>0.00</td><td>29.2</td><td>51.5</td><td>0.411</td><td>0.864</td><td>0.099</td><td>0.000</td><td>0.003</td><td>0.70 1</td><td>0.179</td><td>0.002</td><td>0.320</td><td>0.001</td><td>0.000</td><td>v.d.</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>473</td><td>551</td></tr><tr><td>DX168GY-05</td><td>Qz2 b</td><td>19.9</td><td>19.3</td><td>242</td><td>20.4</td><td>0.00</td><td>50.8</td><td>1.25</td><td>7.195</td><td>0.315</td><td>0.263</td><td>0.000</td><td>0.83 5</td><td>0.393</td><td>0.111</td><td>0.257</td><td>0.038</td><td>0.062</td><td>v.d.</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>472</td><td>550</td></tr><tr><td>DX168GY-06</td><td>Qz2 b</td><td>11.9</td><td>23.6</td><td>126</td><td>7.05</td><td>0.00</td><td>50.5</td><td>0.000</td><td>1.449</td><td>0.030</td><td>0.000</td><td>0.018</td><td>0.85 2</td><td>0.780</td><td>0.484</td><td>0.282</td><td>0.172</td><td>0.000</td><td>v.d.</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>472</td><td>550</td></tr><tr><td>DX168GY-07</td><td>Qz2 b</td><td>15.1</td><td>64.7</td><td>164</td><td>18.7</td><td>75.1</td><td>50.1</td><td>0.355</td><td>4.855</td><td>1.523</td><td>0.111</td><td>0.015</td><td>0.68 9</td><td>0.721</td><td>0.078</td><td>0.207</td><td>0.134</td><td>0.050</td><td>v.d.</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>471</td><td>549</td></tr></table>
<table><tr><td>DX168GY-09</td><td>Qz2 b</td><td>14.6 17.9 147 6.99</td><td>v.d.</td><td>51.5 0.729</td><td>v.d.</td><td>0.179 0.055 0.000</td><td>0.53 1</td><td>0.104 v.d.</td><td>0.248 0.041 0.045</td><td>v.d.</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>473</td><td>551</td></tr><tr><td>DX168GY-10</td><td>Qz2 b</td><td>15.9 3.47 152 3.36</td><td>69.9</td><td>59.7 0.417</td><td>1.602 0.054 0.145</td><td>0.000</td><td>0.63 7</td><td>0.278 0.063 0.168 0.012</td><td>0.003</td><td>v.d.</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>483</td><td>563</td></tr><tr><td>DX168GY-13</td><td>Qz2 b</td><td>14.5 34.2 153 12.7</td><td>34.4</td><td>37.1 0.000</td><td>0.245 0.081 0.546</td><td>0.004</td><td>0.82 8</td><td>0.238 0.051 0.120 0.029</td><td>0.014</td><td>v.d.</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>452</td><td>526</td></tr><tr><td>DX168GY-14</td><td>Qz2 b</td><td>12.4 7.32 110 3.67</td><td>70.6</td><td>41.4 0.000</td><td>1.981 0.000 0.000</td><td>0.009</td><td>0.79 6</td><td>0.221 0.235 0.278 0.029</td><td>0.003</td><td>v.d.</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>459</td><td>534</td></tr><tr><td>DX168GY-18</td><td>Qz2 b</td><td>12.9 1.66 110 1.33</td><td>45.4</td><td>41.4 0.000</td><td>2.381 0.305 0.005</td><td>0.014</td><td>0.65 9</td><td>0.257 0.011 0.168 0.008</td><td>0.000</td><td>v.d.</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>459</td><td>535</td></tr><tr><td>DX168GY-19</td><td>Qz2 b</td><td>18.3 2.64 189 10.4</td><td>32.9</td><td>59.6 0.581</td><td>2.914 0.000 0.288</td><td>0.007</td><td>0.74 9</td><td>0.128 0.009 0.146 0.018</td><td>0.001</td><td>v.d.</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>482</td><td>563</td></tr><tr><td>DX168GY-20</td><td>Qz2 b</td><td>15.5 7.09 159 8.50</td><td>26.3</td><td>59.1 0.000</td><td>1.435 0.000 0.101</td><td>0.008</td><td>0.70 1</td><td>0.140 0.034 0.293 0.014</td><td>0.006</td><td>v.d.</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>482</td><td>562</td></tr><tr><td>DX168GY-21</td><td>Qz2 b</td><td>11.6 8.61 98.1 2.59</td><td>5.86</td><td>48.5 0.199</td><td>0.845 0.118 0.155</td><td>0.003</td><td>0.87 1</td><td>0.197 0.060 0.125 0.010</td><td>0.007</td><td>v.d.</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>469</td><td>547</td></tr><tr><td>DX168GY-22</td><td>Qz2 b</td><td>8.40 31.8 76.1 15.1</td><td>56.8</td><td>42.0 0.967</td><td>3.474 0.399 0.553</td><td>0.014</td><td>1.13 7</td><td>0.155 0.021 0.197 0.007</td><td>0.111</td><td>v.d.</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>460</td><td>536</td></tr><tr><td>DX168GY-25</td><td>Qz2 b</td><td>13.4 2.07 108 1.87</td><td>0.000</td><td>55.7 0.380</td><td>0.835 0.000 0.000</td><td>0.006</td><td>0.72 4</td><td>0.253 0.005 0.180 0.000</td><td>0.001</td><td>v.d.</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>478</td><td>557</td></tr><tr><td>DX168GY-30</td><td>Qz2 b</td><td>12.7 8.04 108 2.58</td><td>4.58</td><td>53.9 0.060</td><td>1.552 0.474 0.004</td><td>0.012</td><td>0.85 8</td><td>0.242 0.121 0.185 0.007</td><td>0.002</td><td>v.d.</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>476</td><td>555</td></tr><tr><td>DX168GY-31</td><td>Qz2 b</td><td>14.4 26.3 132 5.55</td><td>71.6</td><td>53.0 0.872</td><td>0.000 0.229 0.000</td><td>0.000</td><td>0.58 5</td><td>0.522 0.202 0.125 0.163</td><td>0.014</td><td>v.d.</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>475</td><td>553</td></tr><tr><td>DX168GY-33</td><td>Qz2 b</td><td>4.30 154 81.2 18.1</td><td>28.9</td><td>38.4 0.000</td><td>4.785 2.778 0.816</td><td>0.003</td><td>0.85 0</td><td>0.328 0.657 0.003 0.103</td><td>0.266</td><td>v.d.</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>454</td><td>529</td></tr><tr><td>DX168GY-38</td><td>Qz2 b</td><td>14.9 4.05 135 2.80</td><td>41.2</td><td>56.5 0.000</td><td>1.672 0.165 0.000</td><td>0.008</td><td>0.68 0</td><td>0.321 0.094 0.180 0.004</td><td>0.002</td><td>v.d.</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>479</td><td>558</td></tr><tr><td>DX168GY-Q39</td><td>Qz2 b</td><td>14.8 0.99 2 123 3.91</td><td>24.7</td><td>49.9 0.000</td><td>1.374 0.000 0.229</td><td>0.002</td><td>0.80 5</td><td>0.200 0.026 0.199 0.005</td><td>0.004</td><td>v.d.</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>471</td><td>549</td></tr><tr><td>DX168GY-43</td><td>Qz2 b</td><td>16.1 0.12 130 1.43</td><td>69.0</td><td>57.1 0.000</td><td>2.982 0.000 0.000</td><td>0.010</td><td>0.75 7</td><td>0.192 0.005 0.159 0.088</td><td>0.002</td><td>v.d.</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>480</td><td>559</td></tr><tr><td>DX168GY-44</td><td>Qz2 b</td><td>12.9 v.d. 103 0.35</td><td>41.1</td><td>48.3 0.000</td><td>0.334 0.015 0.200</td><td>0.002</td><td>0.60 0</td><td>0.242 0.002 0.170 0.040</td><td>0.003</td><td>v.d.</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>469</td><td>546</td></tr><tr><td>DX168GY-45</td><td>Qz2 b</td><td>16.6 2.54 142 1.55</td><td>53.2</td><td>54.8 0.187</td><td>0.979 0.100 0.000</td><td>0.009</td><td>0.74 7</td><td>0.159 0.011 0.276 0.100</td><td>0.000</td><td>v.d.</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>477</td><td>556</td></tr></table>
<table><tr><td>DX168GY-09</td><td>Qz2 b</td><td>14.6 17.9 147 6.99</td><td>v.d.</td><td>51.5 0.729</td><td>v.d.</td><td>0.179 0.055 0.000</td><td>0.53 1</td><td>0.104 v.d.</td><td>0.248 0.041 0.045</td><td>v.d.</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>473</td><td>551</td></tr><tr><td>DX168GY-10</td><td>Qz2 b</td><td>15.9 3.47 152 3.36</td><td>69.9</td><td>59.7 0.417</td><td>1.602 0.054 0.145</td><td>0.000</td><td>0.63 7</td><td>0.278 0.063 0.168 0.012</td><td>0.003</td><td>v.d.</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>483</td><td>563</td></tr><tr><td>DX168GY-13</td><td>Qz2 b</td><td>14.5 34.2 153 12.7</td><td>34.4</td><td>37.1 0.000</td><td>0.245 0.081 0.546</td><td>0.004</td><td>0.82 8</td><td>0.238 0.051 0.120 0.029</td><td>0.014</td><td>v.d.</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>452</td><td>526</td></tr><tr><td>DX168GY-14</td><td>Qz2 b</td><td>12.4 7.32 110 3.67</td><td>70.6</td><td>41.4 0.000</td><td>1.981 0.000 0.000</td><td>0.009</td><td>0.79 6</td><td>0.221 0.235 0.278 0.029</td><td>0.003</td><td>v.d.</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>459</td><td>534</td></tr><tr><td>DX168GY-18</td><td>Qz2 b</td><td>12.9 1.66 110 1.33</td><td>45.4</td><td>41.4 0.000</td><td>2.381 0.305 0.005</td><td>0.014</td><td>0.65 9</td><td>0.257 0.011 0.168 0.008</td><td>0.000</td><td>v.d.</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>459</td><td>535</td></tr><tr><td>DX168GY-19</td><td>Qz2 b</td><td>18.3 2.64 189 10.4</td><td>32.9</td><td>59.6 0.581</td><td>2.914 0.000 0.288</td><td>0.007</td><td>0.74 9</td><td>0.128 0.009 0.146 0.018</td><td>0.001</td><td>v.d.</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>482</td><td>563</td></tr><tr><td>DX168GY-20</td><td>Qz2 b</td><td>15.5 7.09 159 8.50</td><td>26.3</td><td>59.1 0.000</td><td>1.435 0.000 0.101</td><td>0.008</td><td>0.70 1</td><td>0.140 0.034 0.293 0.014</td><td>0.006</td><td>v.d.</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>482</td><td>562</td></tr><tr><td>DX168GY-21</td><td>Qz2 b</td><td>11.6 8.61 98.1 2.59</td><td>5.86</td><td>48.5 0.199</td><td>0.845 0.118 0.155</td><td>0.003</td><td>0.87 1</td><td>0.197 0.060 0.125 0.010</td><td>0.007</td><td>v.d.</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>469</td><td>547</td></tr><tr><td>DX168GY-22</td><td>Qz2 b</td><td>8.40 31.8 76.1 15.1</td><td>56.8</td><td>42.0 0.967</td><td>3.474 0.399 0.553</td><td>0.014</td><td>1.13 7</td><td>0.155 0.021 0.197 0.007</td><td>0.111</td><td>v.d.</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>460</td><td>536</td></tr><tr><td>DX168GY-25</td><td>Qz2 b</td><td>13.4 2.07 108 1.87</td><td>0.000</td><td>55.7 0.380</td><td>0.835 0.000 0.000</td><td>0.006</td><td>0.72 4</td><td>0.253 0.005 0.180 0.000</td><td>0.001</td><td>v.d.</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>478</td><td>557</td></tr><tr><td>DX168GY-30</td><td>Qz2 b</td><td>12.7 8.04 108 2.58</td><td>4.58</td><td>53.9 0.060</td><td>1.552 0.474 0.004</td><td>0.012</td><td>0.85 8</td><td>0.242 0.121 0.185 0.007</td><td>0.002</td><td>v.d.</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>476</td><td>555</td></tr><tr><td>DX168GY-31</td><td>Qz2 b</td><td>14.4 26.3 132 5.55</td><td>71.6</td><td>53.0 0.872</td><td>0.000 0.229 0.000</td><td>0.000</td><td>0.58 5</td><td>0.522 0.202 0.125 0.163</td><td>0.014</td><td>v.d.</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>475</td><td>553</td></tr><tr><td>DX168GY-33</td><td>Qz2 b</td><td>4.30 154 81.2 18.1</td><td>28.9</td><td>38.4 0.000</td><td>4.785 2.778 0.816</td><td>0.003</td><td>0.85 0</td><td>0.328 0.657 0.003 0.103</td><td>0.266</td><td>v.d.</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>454</td><td>529</td></tr><tr><td>DX168GY-38</td><td>Qz2 b</td><td>14.9 4.05 135 2.80</td><td>41.2</td><td>56.5 0.000</td><td>1.672 0.165 0.000</td><td>0.008</td><td>0.68 0</td><td>0.321 0.094 0.180 0.004</td><td>0.002</td><td>v.d.</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>479</td><td>558</td></tr><tr><td>DX168GY-Q39</td><td>Qz2 b</td><td>14.8 0.99 2 123 3.91</td><td>24.7</td><td>49.9 0.000</td><td>1.374 0.000 0.229</td><td>0.002</td><td>0.80 5</td><td>0.200 0.026 0.199 0.005</td><td>0.004</td><td>v.d.</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>471</td><td>549</td></tr><tr><td>DX168GY-43</td><td>Qz2 b</td><td>16.1 0.12 130 1.43</td><td>69.0</td><td>57.1 0.000</td><td>2.982 0.000 0.000</td><td>0.010</td><td>0.75 7</td><td>0.192 0.005 0.159 0.088</td><td>0.002</td><td>v.d.</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>480</td><td>559</td></tr><tr><td>DX168GY-44</td><td>Qz2 b</td><td>12.9 v.d. 103 0.35</td><td>41.1</td><td>48.3 0.000</td><td>0.334 0.015 0.200</td><td>0.002</td><td>0.60 0</td><td>0.242 0.002 0.170 0.040</td><td>0.003</td><td>v.d.</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>469</td><td>546</td></tr><tr><td>DX168GY-45</td><td>Qz2 b</td><td>16.6 2.54 142 1.55</td><td>53.2</td><td>54.8 0.187</td><td>0.979 0.100 0.000</td><td>0.009</td><td>0.74 7</td><td>0.159 0.011 0.276 0.100</td><td>0.000</td><td>v.d.</td><td>v.d.</td><td>0.5</td><td>1.5</td><td>477</td><td>556</td></tr></table>