# GNSS velocity field in and around Sicily. Insights on the regional tectonic context

Marine Roger

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Marine Roger. GNSS velocity field in and around Sicily. Insights on the regional tectonic context. Ecole normale supérieure - PSL; Université de Strasbourg (Unistra). 2016. hal-05322886

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GNSS velocity field in and around Sicily –
Insights on the regional tectonic context

Marine ROGER

15 June 2016
## SUMMARY

In this report, we present a new study of the Geodynamics of Sicily using an updated solution of GNSS (Global Navigation Satellite System) crustal velocities in and around Sicily obtained from 20 years of GNSS survey. Sicily has a dense spatial coverage of geodetic data which gives a great possibility of understanding motion of Sicily with respect to mainland Italy and the various tectonic blocks around. Since Sicily is located at the boundary between Nubia and Eurasia plates, the new solution also allows to discuss the relative motion between these two major tectonic plates. Here, we explore the new solution through a series of spots at different scales completed with tectonic and seismic data and modelling of some of the largest seismic events in order to understand the seismicity of Sicily and surroundings, as well as crustal deformation around Etna. Significant earthquakes and fault systems have and are still impacting the island. We focus our study on three of these events: (1) the Aeolian-Tindari-Letojanni Fault System (ATLFS) which represents the boundary between the Sicilian block and Calabria and plays a role in earthquake like the one of Messina in 1908; (2) the major earthquake of 1693 near Noto that was followed by a tsunami and which devastated the south eastern Sicily; (3) the 1968 event of Belice, west of Sicily. We discuss each of those events and the crustal motion and deformation around Sicily.

**Keywords:** Geodesy, tectonics, seismicity

## RESUME

Dans ce rapport, nous présentons une nouvelle étude de la Géodynamique de la Sicile utilisant une solution mise à jour des vitesses GNSS (Global Navigation Satellite System) en Sicile et dans les régions avoisinantes obtenues grâce à 20 ans de surveillance géodésique. La Sicile possède une couverture spatiale importante de données géodésiques ce qui permet une étude précise de son mouvement par rapport au reste de l'Italie et aux différents blocs tectoniques l'entourant. La Sicile étant localisée à la frontière entre les plaques Nubie et Eurasie, cette nouvelle solution permet également de discuter le mouvement relatif entre ces deux plaques tectoniques majeures. Ici, nous explorons la nouvelle solution à travers une série de cartes faites à différentes échelles et complétées de données tectoniques et sismiques et de modélisation de certains importants évènements sismiques dans le but de comprendre la sismicité de la Sicile et de ces alentours, ainsi que la déformation crustale au niveau de l'Etna. De majeurs séismes et failles ont impacté et impactent toujours l'île. Nous focalisons notre étude sur trois de ces évènements : (1) le système de failles Aeolian-Tindari-Letojanni (ATLFS) qui représente la frontière entre le bloc sicilien et la Calabre et qui joue un rôle dans les tremblements de terre comme celui de Messine en 1908 ; (2) le séisme majeur de 1693 à proximité de Noto qui a été suivi d'un tsunami et qui a devasté le sud-est de la Sicile ; (3) l'évènement de 1968 à Belice à l'ouest de la Sicile. Nous discutons chacun de ces évènements ainsi que le mouvement et la déformation crustale autour de la Sicile.

**Mots clés:** Géodésie, Tectonique, Sismicité
# Contents

I INTRODUCTION 4

II GNSS DATA 6

1 DATA ANALYSIS 6

2 SICILY WITHIN THE TRANSITION ZONE BETWEEN NUBIA AND EURASIA PLATE 6

2.1 Deformation in the Sicily channel 6

2.2 Consistency of the velocity field when using different hypothesis for the pole of rotation 6

III AROUND SICILY 13

1 SICILY AND THE SURROUNDING BLOCKS 13

2 THE TRANSITION SICILY-CALABRIA 14

3 APULIA, CALABRIA AND THE SOUTHERN APENNINES 21

IV CRUSTAL DEFORMATION INSIDE SICILY 23

1 EXTENSION IN NORTHERN SICILY 24

2 WESTERN SICILY AND THE BELICE LEFT-LATERAL FAULT ZONE 24

3 ETNA 26

4 HYBLEAN PLATEAU AND OFFSHORE FAULTS IN THE IONIAN SEA 26

V CONCLUSION 28

A GNSS DATA 32

B HISTORICAL EARTHQUAKES 42

C TIME SERIES OF RING STATION 44
# I INTRODUCTION

Sicily, located within the Nubia-Eurasia plate boundary, shows a large diversity of seismic- tonic context as depicted by the distribution of the seismicity and the associated focal mech- anisms (Fig.1): compression to the north of the island, several zones with oblique or strike- slip faulting (Aeolian-Tindari-Letojanni Fault System (ATLFS), Belice), extension across the Nebrodi and Peloritani mountains, deep seismicity east of the island in relation with the Cal- abrian subduction, and the existence of active volcanism at Etna, in the Aeolian islands and in the Sicily channel.

<figure><img src="image_2.png" /><figcaption>Figure 1 – Seismicity from the Italian Seismological Instrumental and Parametric Data-Base (http://iside.rm.ingv.it) for the period 1985-2016: white for depth <30 km; yellow for depth between 30 and 150 km; red for depth >150 km and magnitude 2≤Mw≤6.5. Focal mechanisms for the period 1997-2016 and magnitude 3.9≤Mw≤6.5 from the European Regional Centroid Moment Tensor Catalog (http://www.bo.ingv.it/RCMT/searchRCMT.html): red for thrust faulting, green for normal faulting and blue for strike-slip.</figcaption></figure>
Figure 2 shows that the seismicity in-land and around Sicily is located in the crust except near the Messina Strait and north of it, below the Tyrrhenian Basin, where seismicity reaches a depth of 650 km in the Calabrian subduction.

The crustal seismicity corresponds to a wide-range of tectonic regimes:

* Crustal seismicity with compressive focal mechanisms is present in the south of the Tyrrhenian sea and west of the Aeolian Islands, while, immediately to the south, extensive tectonics dominates in Nebrodi and the Peloritani mountains.

* In the east of Sicily, a transition between compressional and extensional zones is delimited by the ATLFS.

* Around the Aeolian Islands, east of Sicily, within the Ionian Sea and from the Malta escarpment until the Sicily channel, the events show a mix of strike-slip and normal mechanisms that indicate a right lateral trans-tensile along the eastern coast of Sicily. The great 1693 earthquake that occured near Syracusa east of Sicily is still a matter of debate but most of the recent publications propose an offshore normal faulting mechanism.

* The Hyblean plateau is seismically stable in comparison to the rest of Sicily with some strike slip mechanisms on (or around) the 'Scicli-Ragusa' Fault System.

The first aspect that will be discussed is the GNSS (Global Navigation Satellite System) data and their processing in order to produce an updated solution of GNSS velocities in and around Sicily. Then we will discuss how this velocity field is related to the shallow (crustal) and deep tectonics and the link between deformation and seismicity. Finally, we will discuss deformation within Sicily: interactions between the Etna volcano and the regional tectonic context, as well as three notable seismic areas: Messina, Noto and Belice.

<figure><img src="image_3.png" /><figcaption>Figure 2 – See caption of Fig. 1.</figcaption></figure>
# II GNSS DATA

## 1 DATA ANALYSIS

We used Global Navigation Satellite System (GNSS) data and published velocities from permanent stations and campaigns located in and around Sicily in an area comprised between 8° and 22° in eastern longitude and 35° and 45° in northern latitude. For the stations of Sicily, Calabria and Aeolian Islands, we calculated our own time series and derived velocities for all stations with available RINEX data. This is the case for part of the RING array and some other stations (IGS, EUREF, MEDSUV project (but restricted to 2005-2011)). We processed the data using the GIPSY 6.4 software (GNSS-Inferred Positioning System and Orbit Analysis Simulation Software). Those stations, calculated by us, correspond to the label "this study" in Table 3 (Appendix A). In Sicily, we also used vectors obtained from campaign stations, several of them having been installed approximately twenty years ago (e.g. Achilli et al. [1995]). Figure 25 (Appendix C) shows the time series obtained by us for some available RING stations of Sicily and southern Calabria <fnref n="1" />. The velocities are determined in the ITRF 2008 geodetic reference frame (Altamimi et al. [2012]). To our own velocities, we added the velocities published in the recent years by several authors (Barreca et al. [2014]; Bonforte et al. [2014]; Devoti et al. [2011]; Métois et al. [2015]; Müller [2011]; Musumeci et al. [2014]; Nocquet [2012]; Ventura et al. [2014]), aligning each of the published solution on our own set of vectors. The analysis of the differences between various published solutions indicates that the average range of variation of the published velocity vectors (determined twice or more) is 0.5 mm.yr⁻<fnref n="1" /> both in east and north components. Most of the authors published uncertainties on their velocities consistent with this figure, and the average uncertainty on the 468 velocities of our Table 3 is 0.3 mm.yr⁻<fnref n="1" /> both in east and north components. We also checked the consistency of our solutions at NOTO and MATE <fnref n="2" /> with those from EUREF and IGS. Figure 9 shows the velocity plotted with respect to Lampedusa, which is considered to be located on the Nubia plate as we discuss in the next section.

## 2 SICILY WITHIN THE TRANSITION ZONE BETWEEN NUBIA AND EURASIA PLATE

### 2.1 Deformation in the Sicily channel

The Sicily channel is a shallow sea domain between Sicily and Tunisia with active seismicity and volcanism (Fig. 1). Strike slip faults prevail in the strait of Sicily with some normal faults in agreement with a transtensive behaviour of tectonic structures (Nocquet [2012], Ventura et al. [2014]).

### 2.2 Consistency of the velocity field when using different hypothesis for the pole of rotation

Relative motion between two plates on a spherical earth can be described as a rotation around an axis through the earth center that pierce the sphere at two opposite points called eulerian or rotation poles. Here, we test two different poles that have been proposed for Nubia (in ITRF 2008 frame) by Altamimi et al. [2012] and Saria et al. [2013].

<footnote n="1">¹To fit the data, we used the formula: $f(x) = f_0 + a.x + b.sin(2.\pi.x/T + \phi)$, that includes the modeling of an annual periodic term, with $f_0$, a, b constants, $\phi$ in radian and T in seconds</footnote>

<footnote n="2">²These two reference stations have been measured for more than two decades.</footnote>
<figure><img src="image_4.png" /><figcaption>Figure 3 – Location of the GNSS stations used to determine the Sicilian pole.</figcaption></figure>

## Sicily: a possible part of Nubia plate ?

We first look at the residual vectors within Sicily. The aim is two-fold: (1) if Sicily belongs to a rigid Nubia plate, then we expect the residuals for stations in Sicily in this frame to be close to zero; (2) if instead Sicily is not attached to Nubia, then systematic residuals should be observed, especially between the west and south-eastern GNSS points.

Using the NUBIA ITRF 2008 pole of Altamimi et al. [2012] (-50.54°N; 99.027°E; 0.262°.Ma⁻¹), we see that none of Sicily areas belong to Africa (Fig.4). Indeed, residuals are all greater than 1 mm.yr⁻¹ with a mean of 2.95 mm.yr⁻¹. Stations systematically move to the East-NorthEast in this reference frame. For instance, the residual at NOTO station is 2.17 mm.yr⁻¹ in East component and 1.20 mm.yr⁻¹ in North component, implying a 2.5 mm.yr⁻¹ motion in the direction N61°E. Sicily thus does not belong to Nubia, and the mean residual motion (2 to 3 mm.yr⁻¹ towards N60°E to N80°E) is consistent and compatible with the present-day opening of the Pelagian graben. Moreover, the fact that residuals do not evolve significantly from West to East, indicates that internal deformation within the Island is small. Deformation within Sicily will be discussed in a further section.
<figure><img src="image_5.png" /><figcaption>Figure 4 – Residual vectors of each Sicilian station for the Nubia’s pole of Altamimi et al. [2012].</figcaption></figure>

Since two poles are available for Nubia in the recent literature (Altamimi et al. [2012] (Fig.5) and by Saria et al. [2013] (Fig.6)), we plotted our GNSS velocity field using both poles. The derived velocity fields can be compared to the velocity field obtained by subtracting Lampedusa motion to all stations, since Lampedusa, located south of the Pelagian grabens, is expected to belong to the African plate.

<figure><img src="image_6.png" /><figcaption>Figure 5 – GNSS velocity field relative to Nubia’s pole of Altamimi et al. [2012] (-50.54°N, 99.027°E, 0.262°.Ma⁻¹). Ellipses represent 1-sigma confidence error regions.</figcaption></figure>
<figure><img src="image_7.png" /></figure>

Figure 6 – GNSS velocity field relative to Nubia’s pole of Saria et al. [2013] (-49.35°N, 99.22°E, 0.265°.Ma⁻¹). Ellipses represent 1-sigma confidence error regions.

We observe very little difference between the velocity fields calculated with the two poles. The motion of Lampedusa in both velocity fields is negligible: with Altamimi's pole, the value in Lampedusa is 0.7 mm.yr⁻¹ east and 0.1 mm.yr⁻¹ north; and with Saria's pole, we find 0.8 mm.yr⁻¹ east and -0.6 mm.yr⁻¹ north. Both values are within the uncertainties, and we conclude that Lampedusa belongs to Nubia.

## Sicily: a rigid micro-plate ?

The next test is to check whether Sicily can be treated as an independant tectonic block. To do so, we used an Excel program written by Nicolas Chamot-Rooke, named Fipole, that finds the best rigid rotation that minimizes the residuals at a given set of stations. Motions at Sicilian stations are best minimized (Fig.7) using the following pole: -57.65°N ; 138.97°E ; 0.396°.Ma⁻¹. The mean residual is 0.36 mm.yr⁻¹. This pole is actually close to the pole of Altamimi et al. [2012], but residuals in Sicily are far much smaller.
<figure><img src="image_8.png" /><figcaption>Figure 7 – GNSS velocity field minimizing Sicily (Pole: -57.65°N; 138.97°E; 0.396°.Ma⁻¹). Ellipses represent 1-sigma confidence error regions.</figcaption></figure>

<figure><img src="image_9.png" /><figcaption>Figure 8 – Residual vectors of each Sicilian station to minimize Sicily.</figcaption></figure>
Discussion about the motion of Sicily in the reference frame of Nubia

Combining the pole of Altamimi et al. [2012] for Nubia and our new pole for Sicily, we obtain Sicily/Nubia pole: 44.47°N; 11.44 °E; 0.1908°.Ma⁻¹. This pole is located near Modena, in the south of the Po plain, north of our study area. In this representation, we find 2.97 mm.yr⁻¹ in the N71.6°E azimuth at NOTO, which can be seen again as a measure of the opening rate and direction of the Pelagian grabens in the Sicily channel. This direction N71° of opening is slightly oblique with respect to the direction of the Pelagian grabens, so that there is a need of a dextral component to accommodate this obliquity, which seems to be observed in marine Geophysics data.

Combining two poles with their uncertainties results in an even larger uncertainty. Precise position of this pole would however be interested for its implications in the Ionian Sea, since the predicted Sicily/Nubia motion is increasing when moving away to the south east. For instance, this pole predicts almost 4 mm.yr⁻¹ in the Ionian Sea, but how this gradient would be accommodated at sea remains unknown. In particular, and this does not account for the relative motion that one may expect between Calabria and Apulia when crossing the northern boundary of the Calabrian subduction in the Taranto gulf.

Considering that Lampedusa belongs to the Nubia's plate, as discussed before, we plot a map (Fig. 9) of the GNSS velocity field in and around Sicily to see the global motion<fnref n="3" />.

<footnote n="3">³In this report, maps are shown in different reference frames to obtain better visualisations, but this does not change the nature of deformation since deformation is frame-independent.</footnote>
<figure><img src="image_10.png" /></figure>

Figure 9 – GNSS velocity field in and around Sicily relative to Lampedusa station assumed to be located on the Nubia plate, thus the vectors represent the motion with respect to Nubia. Ellipses represent 1-sigma confidence error regions. (Map reference of tectonic structures: Rabaute A. and Chamot-Rooke, N. (2014) *Active Tectonics of the Africa-Eurasia Boundary from Algiers to Calabria*, Map at 1 500 000 scale, Paris, ISBN 978-2-9548197-0-9).

In summary, the comparison of Fig. 5, 6 and 9 shows that the velocity field with respect to Lampedusa is about the same on the three maps (i.e the three approaches). So, the hypothesis of Lampedusa belonging to Nubia is validated within the current error bars. Furthermore, few seismicity is present between Tunisia and Sicily in the Pelagian grabens, but not zero, and the azimuth of the relative motion predicted by the models is in good agreement with the transversile grabens as they have been imaged by marine geophysics studies.

This map permits us to see the different blocks present around Sicily: extension in the center of Italy, along the Apennines, extension localized near the Peloritani mounts, compression offshore along the northern coast of Sicily at approximately the latitude of Ustica. Several blocks are present in Sicily: the Hyblean Plateau is relatively stable in comparison with the rest of Sicily in the last 20 years, the west part presents a rotation quasi eastward, the Calabrian block start in Sicily at the level of the ATLFS west of Messina with a movement northeastward in the continuity of the subducting slab.
# III AROUND SICILY

## 1 SICILY AND THE SURROUNDING BLOCKS

At the first order, the GNSS velocities relative to NOTO (Fig.10) show that Sicily is surrounded by three major units:

* to the south-west, the Nubia plate to which the GNSS station LAMP is considered to be attached, with a small amount of right lateral trans-tensile strain in the Sicily channel as shown by the velocity of Pantelleria and almost no relative velocity between Malta and the south-east of Sicily. This was discussed in the previous section;

* to the north-west, the European plate to which Sardinia is considered to be attached with Ustica being in the transition zone as shown by its GNSS velocity and the focal mechanisms (see also the previous section);

* to the east the Calabria-Apulia block(s).

In addition, three obvious deforming zones are observed inside Sicily:

* the deformation on and around Etna volcano;

* an inland extension along the north coast of Sicily, in particular across the Nebrodi mountains;

* a zone of left lateral motion in the Belice area, west of the island.

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

Figure 10 – GNSS velocity field relative to NOTO station (Southeastern Sicily). Ellipses represent 1-sigma confidence error regions. See caption of Fig.1 for the focal mechanisms and Fig.9 for tectonic structures. Cross section A-A' (Fig.12).
## 2 THE TRANSITION SICILY-CALABRIA

### Active faulting at the boundary Sicily-Calabria

Several active faults play an important role in the seismo-tectonics of the north-east of Sicily: the Taormina Fault system (TFS) and the " Aeolian-Tindari-Letojanni" fault system (ATLFS) (De Guidi et al. [2012]; Palano et al. [2015]) that continues offshore to the Aeolian Islands. The ATLFS is considered to be composed of several segments:

* the north one starts in the Aeolian Islands and continues north to the Gulf of Patti and is dominated by dextral lateral-slip;

* the central one starts north-east Sicily on-shore near Tindari and, continues south until the watershed of Peloritani mounts and is dominated by normal faulting with minor dextral lateral slip (Orecchio et al. [2014]; Presti et al. [2013]);

* the south part, not clearly visible in the field, with little seismic activity according to the catalogs of earthquakes, goes from the central Peloritani mounts to the Ionian coast of Sicily near Letojanni.

This ATLFS fault system is composed of right-lateral and extensional faults. It makes the transition between the eastern extensional domain and the western collisional domain of Sicily, and separates the block Sicily and the block Calabria. It is considered by several authors (De Guidi et al. [2012]; Orecchio et al. [2014]; Palano et al. [2015]; Scarfi et al. [2016]) as a lateral slab tear separating the ongoing subduction-rollback processes of the Ionian oceanic to the east from the still active continental collision to the west, the slab provokes non uniform transformations on the ATLFS.

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

Figure 11 – GNSS velocity field relative to NOTO station. Ellipses represent 1-sigma confidence. SRTM data was used for topography. See caption of Fig.1 for the focal mechanisms and Fig.9 for tectonic structures; focal mechanism of the 28 December 1908 of Messina collected from Gasparini,1985.
Current velocity of the ATLFS from GPS observations

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

Figure 12 – A-A' cross section (see location on Fig.10). Blue points are for parallel components of the velocity (mm.yr⁻¹) and red points for perpendicular components. Error bars were plotted for a family of points in order not to saturate the figure. This have the same amplitude for the other data.

Figure 12 shows a projection of the velocities (relative to Noto) along the A-A' profile oriented N30°E. This azimuth is the one that minimizes the velocities parallel to the profile. The figure shows a segmentation in two blocks: "Sicily" west of the ATLFS and "Calabria" east of it, with a boundary between 15.1°E around Tindari and 15.3°E around Taormina.

In the parallel component, both sides are well minimized within ~0.1 mm.yr⁻¹. In the perpendicular component, the "Sicily" block has an average perpendicular velocity of -0.35±0.2 mm.yr⁻¹ while the "Calabria" side is at -2.8±0.2 mm.yr⁻¹, with therefore an offset across the Aeolian-Letojanni-Tindari fault of 2.2±0.2 mm.yr⁻¹. To estimate this offset, we made two different hypothesis: one assuming a linear slope of the perpendicular component as function of longitude in Calabria (red curve), the other assuming a constant value (pink curve).

Projected on the ATLFS (assuming a N25°W azimuth for this fault), this offset corresponds to 1.8±0.2 mm.yr⁻¹ of right lateral strike slip across the fault and 1.3±0.2 mm.yr⁻¹ of extension across the fault. This last value will be discussed in more detail later. It is consistent with the one found along the N105°E section crossing the fault zone of the 1908 Messina earthquake.

<figure><img src="image_14.png" /></figure>
The geodetic data agree well with the position of the ATLFS predicted in literature.

## The 1908 Messina earthquake and associated fault(s)

On 1908 December 28, a major earthquake occured with a magnitude of ~7 in the Messina strait and triggered a devastating tsunami (Aloisi et al. [2012]).

In order to understand this earthquake and its place in the regional tectonic context, we modeled the fault responsible for this event inverting the levelling data of Loperfido [1909] using as forward model, assuming the dislocation of an rectangular fault with homogeneous slip buried in an homogeneous and elastic half space (Okada model). We used a rigidity of 30 MPa for the crust. The fault parameters estimated in this inversion are presented in Table 1. The comparison of the observations and the model (Fig.13B) shows that the Loperfido data's constraint well and in a consistent way the model for both the spatial and geometric parameters of the fault and the amplitude of the slip. Our inversion predicts a significant amount of strike-slip.

<figure><img src="image_15.png" /><figcaption>Figure 13 – A. Overview of the elevation changes measured by geodetic levelling by Loperfido [1909] following the 1908 earthquake (in cm) (from Pino et al. [2009]). B. Comparison between the observed levelling data (Loperfido [1909]) and our model.</figcaption></figure>
<table><caption>Table 1 – Parameters used for the modelling of the fault of Messina 1908.</caption><thead><tr><th>Parameters</th><th>MES08</th><th>INTER1 SHALLOW</th><th>INTER2 DEEP</th></tr></thead><tbody><tr><td>X<sub>center</sub></td><td>545100 m</td><td>541800 m</td><td>565200 m</td></tr><tr><td>Y<sub>center</sub></td><td>4216200 m</td><td>4217200 m</td><td>4211000 m</td></tr><tr><td>Depth top</td><td>2 km</td><td>0 km</td><td>14 km</td></tr><tr><td>Azimuth</td><td>15°</td><td>15°</td><td>15°</td></tr><tr><td>Dip</td><td>30°</td><td>30°</td><td>30°</td></tr><tr><td>Length</td><td>32 km</td><td>infinit</td><td>infinit</td></tr><tr><td>Width</td><td>24 km</td><td>0 km</td><td>infinit</td></tr><tr><td>Strike slip</td><td>-0,230 m</td><td>-0,230 m</td><td>-0,230 m</td></tr><tr><td>Dip slip</td><td>1,450 m</td><td>1,450 m</td><td>1,450 m</td></tr><tr><td>M<sub>0</sub> = μ.s.LH<sup>a</sup></td><td>3,34.10<sup>19</sup> N.m</td><td></td><td></td></tr><tr><td>M<sub>w</sub> = 2/3.log<sub>10</sub>(M<sub>0</sub>) – 10,7<sup>b</sup></td><td>7</td><td></td><td></td></tr></tbody></table>

<figure><img src="image_16.png" /><figcaption>Figure 14 – Location of the fault of the Messina earthquake of 1908 fitting best our model (cf Google earth). Location of the ATLFS. The deformation at the junction Sicily-Calabria is partitioned between the ATLFS and the Messina graben. The low level of activity of the ATLFS during the XX<sup>th</sup> century might be due to the stress drop in the Peloritani mountains, i.e a transient consequence of the 1908 Messina earthquake.</figcaption></figure>

<footnote><sup>a</sup>M<sub>0</sub>: seismic moment (N.m), μ=30 GPa: shear modulus of the rocks involved in faulting, s: average displacement on the dislocation, L: length, H: downdip height of the dislocation along which faulting occured (Aki and Richards [2002]).</footnote>

<footnote><sup>b</sup>Moment magnitude (Hanks and Kanamori [1979])</footnote>
Strain partitioning between the Aeolian-Letoianni-Tindari and the Messina-Reggio
Calabria faults at the boundary between Sicily and Calabria and inferred recurrence time
of large earthquakes

The combination of the present GNSS velocities in the area and the constraints given by the 1908 earthquake indicate that the strain is partitioned in north-east Sicily with a major component of right lateral strike-slip, and minor but significant extension, across the ATLFS, and a secondary major fault zone in the Messina strait, which is an asymmetric graben, with predominant normal faulting and a minor component of right lateral strike slip. The interseismic strain accumulation deduced from the GNSS velocities in the area of the 1908 earthquake (Fig.16) is consistent with a recurrence period of earthquakes of 320 years and with a corresponding strain accumulation of 2 mm.yr⁻¹ across the fault zone which is thus only a small part of the overall 13 mm.yr⁻¹ extension across the entire boundary between Sicily and Calabria.

To better understand how this earthquake and its fault are linked with the ATLFS, we made a map (Fig.15) with GNSS velocities relative to Calabria. As discussed in the previous section, we see that around 15.2° in longitude, there is an abrupt change of the orientation of vectors, this position corresponds to the ATLFS (as previously saw on the cross section A-A', Fig.12).

<figure><img src="image_17.png" /><figcaption>Figure 15 – GNSS velocity field relative to Calabria and position of the ATLFS. Ellipses represent 1-sigma confidence.</figcaption></figure>

To pass from the co-seismic to the inter-seismic and long term, first, we studied the co-seismic
period and compare our fault plane (east-dipping plane) with the models proposed by other
authors (Aloisi et al. [2012]; Valensise and Pantosti [1992]; Pino et al. [2009]). Then, to model the inter-seismic period, we added two faults of infinit length to simulate the shallow and deep aseismic motions: a shallow fault at the north-west of the fault from the surface to 2 km of depth and a deep one starting at 14 km of depth at the south-east, and assign to those faults a steady slip during the inter-seismic period.

When compared to the present GPS velocities, the inter-seismic simulation indicates a recurrence period of the Messina earthquake of 320 years, with an extension rate across the fault of 2.4 mm.yr⁻¹. We see that the partitioning is almost separated equally between the ATLFS and the fault of Messina: 1.3 mm.yr⁻¹ for the ATLFS and 1.1 mm.yr⁻¹ for the fault of Messina. Furthermore, the spatial wavelength of the interseismic is wide and encompasses the area of the ATLFS. Therefore, there is an imbrication of the ATLFS and Messina faults when one considers the strain accumulation over the long term that will eventually (or not) result into earthquakes. The Aeolian-Tindari-Letojanni fault system plays in fact a major role for the genesis of the Messina earthquake. We observe on the graph of the East component that there is almost no extension at the east of the fault. So, if the ATLFS was not there, the recurrence time of this earthquake would be of thousands of years.

There is a partitioning between the ATLFS, strike slip and the Messina fault, normal fault.

<figure><img src="image_18.png" /><figcaption>Figure 16 – Co- and inter-seismic graph of the Messina earthquake of 1908, East component. The 1908 earthquake is predominantly normal on a low angle fault, and the ATLFS is trans-tensile. The model for the 1908 earthquake best fits with a crust being brittle until 14 km of depth. The modelled inter-seismic motion is clearly long wavelength and implies including the ATLFS in the overall loading process eventually producing earthquakes in the Messina strait.</figcaption></figure>
<figure><img src="image_19.png" /></figure>

Figure 17 – Co- and inter-seismic modelled motions for the Messina earthquake of 1908, in the north component along the B-B' section. Present GNSS velocities are plotted with the assumption of 320 years of recurrence time for the Messina earthquake (see previous figure).
3 APULIA, CALABRIA AND THE SOUTHERN APENNINES

<figure><img src="image_20.png" /><figcaption>Figure 18 – Velocity field with respect to Basilicata (MATE) and western Puglia. Ellipses represent 1-sigma confidence. See caption of Fig.1 for the focal mechanisms. Cross section C-C' (see Fig.19).</figcaption></figure>

With respect to the surroundings, we observe little internal deformations in Puglia, Basilicata and Calabria. The extension across the southern Apennines is clearly visible until the gulf of Policastro to the south (~40° of latitude), with an amplitude of ~3 mm.yr⁻¹ across the Irpinia mountains where the large 1980 earthquake occured. Further south, e.g. around Castro Villari, Cosenza there is not any more extension perpendicular to the Apennines and the best fitting azimuth of the extension is now N114°E, e.g. an azimuth consistent with the orientation of the Calabrian subduction. Figure 19 shows a cross section of the velocities parallel and perpendicular to this azimuth of N114°E. The transition between the Apennines extension and the Calabrian extension is located around the gulf of Policastro as written above. In the eastern part of the section, the azimuth of the extension is parallel to the section with a total offset of 2 mm.yr⁻¹ from the Tyrrhenian to the Ionian coast across the Sila mountains. In Apulia, a gradi-
ent in the C-C' azimuth is visible despite the fact that Apulia is located north of the Calabrian subduction arc. As already written, this fact requires further explanations.

<figure><img src="image_21.png" /></figure>

Figure 19 – C-C' section across northern Calabria (Fig.18). Blue points are for parallel component of the velocity (mm.yr⁻¹) and red points for the perpendicular component.
# IV CRUSTAL DEFORMATION INSIDE SICILY

Zooming inside Sicily (Fig.21), there is evidence of significant internal deformations in several places of the island. The largest deforming area is by far the Etna area, and in particular the sliding east side of the volcano.

On the north-east, we already analyzed (section III.2) the transition between Sicily and Calabria, about 40 km further to the west of the Messina strait, along the Aeolian-Tindari-Letojanni fault.

To the west, a deformation area of interest is present with the event of 1968 near Belice. Several major historic earthquakes have affected Sicily (e.g. Noto 1693, Catania 1169, Messina 1908), and several other of minor magnitudes have occurred during the XX^th^ century (e.g. Belice 1968, Carlentini 1990).

<figure><img src="image_22.png" /><figcaption>Figure 20 – Map of historical earthquakes of Sicily. See Table 4 in Appendix B.</figcaption></figure>

The geometry and exact location of each historical event is not well defined. However, many studies exist and their overall conclusions coincide (Barreca et al. [2014]; Lavecchia et al. [2007]): events of Belice 1968, Catanese 1818, Mineo 1624 and Central Sicily near Caltanissetta 361 are defined as thrust faults. Shallow compressional events dominate for Mineo and deep compressional events for the three others.
<figure><img src="image_23.png" /></figure>

Figure 21 – GNSS velocity field relative to the NOTO station. Ellipses represent 1-sigma confidence error regions. SRTM data was used for topography. See caption of Fig.1 for the focal mechanisms and Fig.9 for tectonic structures.

# 1 EXTENSION IN NORTHERN SICILY

On the Tyrrhenian side of the coast of Sicily, on the north side of the Peloritani monts, there is an extension of about 1.5 mm.yr⁻¹ toward north. On the other hand, at the latitude of Ustica, in the sea, compressional movements are present with a southward convergence of 2.7 mm.yr⁻¹. I have not analyzed this area in more details in this work.

# 2 WESTERN SICILY AND THE BELICE LEFT-LATERAL FAULT ZONE

In order to compare the present GNSS velocity field and the known seismicity of in-land Sicily, we added to our study historical seismic data: data collected on the Catalogue of Strong Earthquakes in Italy (CFTI, http://storing.ingv.it/cfti4med/) and thanks to the studies of Lavecchia et al. [2007] and Anderson and Jackson [1987], from year 17 A.D. to 2002 and for magnitudes above 4.

Before 1968 Belice's earthquake, the west side of Sicily was not depicted as seismically active. In 1968, this area endured an earthquake sequence of four mainshocks with the major one, very
shallow (3 km of depth) of a magnitude 5.5. This Belice event was more probably caused by a thrust fault oriented east-west, although there are also interpretations involving a north-south right lateral faulting along a lithospheric transcurrent fault system (Lavecchia et al. [2007]; Barreca et al. [2014]; Calo and Parisi [2014], Di Stefano et al. [2015]). In fact, both interpretations might be correct if one considers that the Belice area is a small compressive transition zone within a regional strike-slip zone as depicted by the GNSS velocities. In practice, to determine the most probable solution, we would need to better identify the seismogenic structures, but as explained Barreca et al. [2014], many deformation occurred recently, so fault scarps cannot be observed. However, this seismic event was a very important one that destroyed many villages and with a distribution of events along the south_west-north_east oriented Belice River Valley.

<figure><img src="image_24.png" /></figure>

Figure 22 – GNSS velocity field relative to NOTO station. Ellipses represent 1-sigma confidence. SRTM data was used for topography. See caption of Fig.1 for the focal mechanisms and seismicity, and Fig.9 for tectonic structures.
## 3 ETNA

Mount Etna's case differs totally from the rest of Sicily. An important diversity of velocity vector is present around the volcano. An extension in all directions can be seen with a major displacement in the east flank, about three times the size of western vectors.

To better understand Etna's situation and his impact on the rest of Sicily, we have studied some time series of station from the RING network, we selected stations on all Sicily and some on the Calabrian block, the closest one from the volcano is GALF (See Appendix C Fig.25). We see that the temporal changes of deformations at Etna can affect significantly GNSS points until distances of 40-50 km of the volcano center, i.e ~20 km out of the volcano base. GNSS points located in this "far field" from the volcano might be of great interest for the understanding of the deep deformations beneath Etna.

## 4 HYBLEAN PLATEAU AND OFFSHORE FAULTS IN THE IONIAN SEA

<figure><img src="image_25.png" /></figure>

Figure 23 - Velocities with respect to NOTO station. Ellipses represent 1-sigma confidence. SRTM data was used for topography. See caption of Fig.1 for the focal mechanisms and Fig.9 for tectonic structures

The Hyblean plateau area, especially the east, is the place of ones of the most important known earthquakes in Sicily like the 1169 and 1693 ($M_w$ = 7.4) or the moderate 1990 one ($M_w$ = 5.4). It is composed of two blocks (west and east), separated by the Scicli-Ragusa Fault System. To the east, the Hyblean-Maltese Escarpment Fault System is the boundary with the Ionian basin (Mattia et al. [2012]; Scarfi et al. [2012]).

According to the present GNSS velocities, the Hyblean plateau does not have large strain
changes and no major earthquake since the earthquake of 1818 ($M_w$ = 6) (Musumeci et al. [2014]; Bonforte et al. [2014]).

All characteristics of the earthquakes of 1169 and 1693 are not well understood yet, but the tsunami observations and model is a strong constraint for the location of the 1693 one (Branca et al. [2015]). The hypothesis of on-shore active contractional structures bordering the northern margin of the Hyblean plateau is less probable as it cannot explain the tsunami.

In figure 24, we show a location of the possible fault of the 1693 earthquake modified from that of Argnani et al. [2012]. We propose a longer fault with less slip (3.5 m instead of 5 m) but same low dip angle (30°). It would be interesting to test models with steep dip angle (70°) that would be more compatible with the geometry of the off-shore faults.

<figure><img src="image_26.png" /><figcaption>Figure 24 – Map of the fault responsible of the earthquake of 1693 near Noto (cf. Google earth).</figcaption></figure>

<table><thead><tr><th>Parameters</th><th>NOTO 1693</th></tr></thead><tbody><tr><td>X<sub>center</sub></td><td>536000 m</td></tr><tr><td>Y<sub>center</sub></td><td>4124000 m</td></tr><tr><td>Depth top</td><td>0 km</td></tr><tr><td>Azimuth</td><td>345°</td></tr><tr><td>Dip</td><td>30°</td></tr></tbody></table>

<table><caption>Table 2 – Parameters for the modelling of the 1693 fault from Argnani et al. [2012].</caption><tr><td>Length</td><td>40 km</td></tr><tr><td>Width</td><td>16 km</td></tr><tr><td>Strike slip</td><td>3,500 m</td></tr><tr><td>Dip slip</td><td>0 m</td></tr><tr><td>M<sub>0</sub></td><td>7.10<sup>19</sup> N.m</td></tr><tr><td>M<sub>w</sub></td><td>7.4</td></tr></table>
# V CONCLUSION

I present an updated map of GNSS velocities in and around Sicily that reveals a sharper image of the tectonic blocks composing Sicily and the fragmentation in Central Mediterranean along the Nubia-Eurasia boundary plate. Geodetic data combined with seismic data show that the Sicily domain is fragmented into three smaller tectonic blocks: the west, the south-east and the east side with the start of Calabria.

The main findings of my study can be summarized as follows:

* firstly, there is a relative motion of Sicily with respect to Nubia of $2.7\pm0.5$ mm.yr$^{-1}$ in the $N70^\circ$ direction which produces the current opening of the Pelagian grabens;

* secondly, our study sheds light on the Aeolian-Tindari-Letojanni fault system: its location, its strike slip behaviour and its role in seismic event such as the earthquake of Messina in 1908. The proposed model suggests a normal fault with minor right lateral strike slip for this event toward east and next to the Sicilian coast;

* thirdly, the Belice area, west of Sicily, is hard to work on because of the geology and the lack of good data for the 1968 earthquake but thanks to the GNSS data and also to interferometry data recently published, the event of 1968 would probably be caused by a thrust fault;

* fourthly, the hyblean plateau has a low seismic activity, low strain changes as revealed by GNSS and the major event of 1693 was most probably caused by a fault off-shore rather than in-land;

* finally, around Etna, crustal deformation is completely different from the rest of Sicily: major extension is localized at the east of the volcano and because of the breathing of the structure, the area around the volcano is disturbed and the analysis of this part of Sicily needs more analysis. Understanding deep Etna processes requires GNSS stations located outside the volcano edifice and the motion of those stations, for inferring the volcanic processes, has to be well decoupled from the local and large scale tectonics motions. The west and south of Etna are best adapted for such studies, while to the north the tectonics of the ATLFS and Peloritan would contaminate the signal.
# ACKNOWLEDGMENTS

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Brunella Mastrolembo Ventura, Enrico Serpelloni, Andrea Argnani, Alessandro Bonforte, Roland Bürgmann, Marco Anzidei, Paolo Baldi, and Giuseppe Puglisi. Fast geodetic strain-rates in eastern sicily (southern italy): New insights into block tectonics and seismic potential in the area of the great 1693 earthquake. *Earth and Planetary Science Letters*, 404:77–88, 2014.
A GNSS DATA

<table><thead><tr><th>N</th><th>Lon</th><th>Lat</th><th>V<sub>E</sub></th><th>V<sub>N</sub></th><th>σ<sub>E</sub></th><th>σ<sub>N</sub></th><th>Site</th><th>Reference</th></tr><tr><th></th><th>°</th><th>°</th><th>mm.yr<sup>-1</sup></th><th>mm.yr<sup>-1</sup></th><th>mm.yr<sup>-1</sup></th><th>mm.yr<sup>-1</sup></th><th></th><th></th></tr></thead><tbody><tr><td>1</td><td>12,606</td><td>35,5</td><td>19,7</td><td>18,6</td><td>0,2</td><td>0,2</td><td>LAMP</td><td>1</td></tr><tr><td>2</td><td>14,526</td><td>35,838</td><td>21,2</td><td>19,7</td><td>0,2</td><td>0,2</td><td>MALT</td><td>6</td></tr><tr><td>3</td><td>14,497</td><td>35,885</td><td>20,4</td><td>19,1</td><td>0,4</td><td>0,4</td><td>EG34</td><td>6</td></tr><tr><td>4</td><td>14,796</td><td>36,731</td><td>19,8</td><td>19,7</td><td>0,6</td><td>0,6</td><td>POZZ</td><td>5</td></tr><tr><td>5</td><td>14,707</td><td>36,794</td><td>21,6</td><td>19,3</td><td>0,3</td><td>0,3</td><td>HSCI</td><td>6</td></tr><tr><td>6</td><td>11,971</td><td>36,811</td><td>21,8</td><td>16,6</td><td>0,4</td><td>0,4</td><td>PZIN</td><td>3</td></tr><tr><td>7</td><td>11,95</td><td>36,83</td><td>21,4</td><td>16,7</td><td>0,5</td><td>0,5</td><td>PANT</td><td>7</td></tr><tr><td>8</td><td>14,99</td><td>36,876</td><td>21,2</td><td>19,8</td><td>0,1</td><td>0,1</td><td>NOT1</td><td>6</td></tr><tr><td>9</td><td>14,783</td><td>36,959</td><td>21</td><td>19,7</td><td>0,2</td><td>0,2</td><td>HMDC</td><td>6</td></tr><tr><td>10</td><td>15,122</td><td>36,96</td><td>21,2</td><td>20</td><td>0,3</td><td>0,3</td><td>HAVL</td><td>6</td></tr><tr><td>11</td><td>14,897</td><td>37,054</td><td>21,5</td><td>20,1</td><td>0,5</td><td>0,5</td><td>PLZA</td><td>5</td></tr><tr><td>12</td><td>15,282</td><td>37,076</td><td>20,6</td><td>18,5</td><td>0,4</td><td>0,4</td><td>SIRC</td><td>6</td></tr><tr><td>13</td><td>14,993</td><td>37,093</td><td>21,7</td><td>19,6</td><td>0,3</td><td>0,3</td><td>IP21</td><td>6</td></tr><tr><td>14</td><td>15,223</td><td>37,151</td><td>21</td><td>18,2</td><td>0,6</td><td>0,6</td><td>IP19</td><td>2</td></tr><tr><td>15</td><td>15,076</td><td>37,158</td><td>21,3</td><td>19,6</td><td>0,3</td><td>0,3</td><td>SSYX</td><td>6</td></tr><tr><td>16</td><td>14,716</td><td>37,177</td><td>20,3</td><td>19</td><td>0,6</td><td>0,6</td><td>HVZN</td><td>5</td></tr><tr><td>17</td><td>14,938</td><td>37,184</td><td>20,4</td><td>20,9</td><td>0,5</td><td>0,5</td><td>IP16</td><td>9</td></tr><tr><td>18</td><td>14,94</td><td>37,184</td><td>22,8</td><td>19,1</td><td>0,6</td><td>0,6</td><td>IP10</td><td>6</td></tr><tr><td>19</td><td>14,516</td><td>37,206</td><td>22,4</td><td>19,6</td><td>0,5</td><td>0,5</td><td>CLTG</td><td>5</td></tr><tr><td>20</td><td>15,114</td><td>37,215</td><td>22,6</td><td>19,9</td><td>0,3</td><td>0,3</td><td>IP12</td><td>2</td></tr><tr><td>21</td><td>14,362</td><td>37,223</td><td>21</td><td>19,8</td><td>0,2</td><td>0,2</td><td>RAFF</td><td>1</td></tr><tr><td>22</td><td>14,889</td><td>37,234</td><td>21,8</td><td>20,8</td><td>0,5</td><td>0,5</td><td>IP14</td><td>2</td></tr><tr><td>23</td><td>15,256</td><td>37,241</td><td>20,9</td><td>19</td><td>0,3</td><td>0,3</td><td>ICRC</td><td>6</td></tr><tr><td>24</td><td>14,989</td><td>37,248</td><td>22,7</td><td>20,2</td><td>0,6</td><td>0,6</td><td>IPNC</td><td>2</td></tr><tr><td>25</td><td>14,879</td><td>37,249</td><td>23,6</td><td>19,1</td><td>0,5</td><td>0,5</td><td>ICDR</td><td>2</td></tr><tr><td>26</td><td>15,025</td><td>37,269</td><td>21,7</td><td>25,1</td><td>0,5</td><td>0,5</td><td>IP13</td><td>9</td></tr><tr><td>27</td><td>15,201</td><td>37,282</td><td>21,7</td><td>19,6</td><td>0,3</td><td>0,3</td><td>IP10</td><td>6</td></tr><tr><td>28</td><td>15,032</td><td>37,283</td><td>22,2</td><td>18,7</td><td>0,4</td><td>0,4</td><td>HCRL</td><td>6</td></tr><tr><td>29</td><td>15,155</td><td>37,286</td><td>21,1</td><td>19,9</td><td>0,3</td><td>0,3</td><td>HAGA</td><td>6</td></tr><tr><td>30</td><td>15,105</td><td>37,299</td><td>22,1</td><td>20,7</td><td>1,4</td><td>1,4</td><td>IGAT</td><td>9</td></tr><tr><td>31</td><td>15,123</td><td>37,303</td><td>21,9</td><td>19,8</td><td>0,3</td><td>0,3</td><td>IP09</td><td>6</td></tr><tr><td>32</td><td>15,015</td><td>37,308</td><td>21,8</td><td>20,8</td><td>0,5</td><td>0,5</td><td>ISLI</td><td>6</td></tr><tr><td>33</td><td>13,669</td><td>37,318</td><td>20,9</td><td>17,3</td><td>0,2</td><td>0,3</td><td>FVRA</td><td>3</td></tr><tr><td>34</td><td>14,754</td><td>37,319</td><td>21,9</td><td>19,9</td><td>0,3</td><td>0,3</td><td>IM02</td><td>6</td></tr><tr><td>35</td><td>14,909</td><td>37,33</td><td>22,4</td><td>20,4</td><td>0,3</td><td>0,3</td><td>IRNE</td><td>6</td></tr><tr><td>36</td><td>14,992</td><td>37,334</td><td>22,3</td><td>20,4</td><td>0,6</td><td>0,6</td><td>ISCP</td><td>2</td></tr><tr><td>37</td><td>15,026</td><td>37,334</td><td>21,2</td><td>19,7</td><td>0,6</td><td>0,6</td><td>IMTR</td><td>6</td></tr><tr><td>38</td><td>14,962</td><td>37,347</td><td>21,9</td><td>20,2</td><td>0,4</td><td>0,4</td><td>IP06</td><td>6</td></tr><tr><td>39</td><td>14,872</td><td>37,349</td><td>21,3</td><td>19,3</td><td>0,5</td><td>0,5</td><td>IP07</td><td>2</td></tr><tr><td>40</td><td>14,872</td><td>37,349</td><td>21,2</td><td>19</td><td>0,5</td><td>0,5</td><td>HLNI</td><td>9</td></tr><tr><td>41</td><td>15,048</td><td>37,38</td><td>21,8</td><td>19,6</td><td>0,3</td><td>0,5</td><td>IAZZ</td><td>6</td></tr><tr><td>42</td><td>15,065</td><td>37,405</td><td>16,4</td><td>21,4</td><td>0,5</td><td>0,5</td><td>IP03</td><td>9</td></tr><tr><td>43</td><td>14,794</td><td>37,405</td><td>21,4</td><td>17,7</td><td>0,7</td><td>0,7</td><td>P04</td><td>6</td></tr><tr><td>44</td><td>14,937</td><td>37,429</td><td>20,9</td><td>18,2</td><td>0,5</td><td>0,5</td><td>IM01</td><td>9</td></tr><tr><td>45</td><td>14,651</td><td>37,504</td><td>21,7</td><td>19,4</td><td>0,5</td><td>0,5</td><td>JUDI</td><td>5</td></tr><tr><td>46</td><td>13,08</td><td>37,512</td><td>21</td><td>18,3</td><td>0,4</td><td>0,4</td><td>SCIA</td><td>6</td></tr></tbody></table>
<table><tr><td>47</td><td>15,082</td><td>37,514</td><td>23,4</td><td>17</td><td>0,3</td><td>0,3</td><td>EIIV</td><td>1</td></tr><tr><td>48</td><td>14,274</td><td>37,57</td><td>21,2</td><td>19</td><td>0,3</td><td>0,3</td><td>ENNA</td><td>1</td></tr><tr><td>49</td><td>12,836</td><td>37,587</td><td>20,7</td><td>18,7</td><td>0,8</td><td>0,8</td><td>SEL1</td><td>4</td></tr><tr><td>50</td><td>14,712</td><td>37,596</td><td>20,9</td><td>17,6</td><td>0,3</td><td>0,4</td><td>ECNV</td><td>1</td></tr><tr><td>51</td><td>15,02</td><td>37,614</td><td>25,3</td><td>8,9</td><td>0,4</td><td>0,4</td><td>ENIC</td><td>1</td></tr><tr><td>52</td><td>14,777</td><td>37,632</td><td>20,3</td><td>19,9</td><td>0,5</td><td>0,5</td><td>9510</td><td>6</td></tr><tr><td>53</td><td>14,057</td><td>37,647</td><td>21,9</td><td>17,2</td><td>0,2</td><td>0,2</td><td>RESU</td><td>3</td></tr><tr><td>54</td><td>12,766</td><td>37,648</td><td>21,4</td><td>18,3</td><td>0,8</td><td>0,8</td><td>BCMA</td><td>4</td></tr><tr><td>55</td><td>20,808</td><td>37,655</td><td>9,5</td><td>-0,9</td><td>0,3</td><td>0,3</td><td>KERI</td><td>7</td></tr><tr><td>56</td><td>14,913</td><td>37,686</td><td>12,5</td><td>7,3</td><td>0,3</td><td>0,3</td><td>ECHR</td><td>1</td></tr><tr><td>57</td><td>15,083</td><td>37,691</td><td>35,5</td><td>3,2</td><td>0,3</td><td>0,3</td><td>EC10</td><td>1</td></tr><tr><td>58</td><td>14,975</td><td>37,693</td><td>21,5</td><td>15,9</td><td>0,4</td><td>0,4</td><td>ENAV</td><td>1</td></tr><tr><td>59</td><td>15,027</td><td>37,693</td><td>31,2</td><td>9,3</td><td>0,4</td><td>0,4</td><td>ESPC</td><td>1</td></tr><tr><td>60</td><td>15,161</td><td>37,702</td><td>51,6</td><td>-5,6</td><td>0,3</td><td>0,3</td><td>EBAG</td><td>1</td></tr><tr><td>61</td><td>14,566</td><td>37,711</td><td>20,6</td><td>18,8</td><td>0,3</td><td>0,3</td><td>GALF</td><td>1</td></tr><tr><td>62</td><td>14,998</td><td>37,719</td><td>29,3</td><td>4</td><td>0,4</td><td>0,4</td><td>EINT</td><td>1</td></tr><tr><td>63</td><td>15,09</td><td>37,736</td><td>45,4</td><td>-4</td><td>0,4</td><td>0,4</td><td>EMFN</td><td>1</td></tr><tr><td>64</td><td>14,987</td><td>37,744</td><td>30,1</td><td>11,6</td><td>0,4</td><td>0,4</td><td>ECPN</td><td>1</td></tr><tr><td>65</td><td>12,716</td><td>37,745</td><td>20</td><td>17,4</td><td>0,8</td><td>0,8</td><td>TLIP</td><td>4</td></tr><tr><td>66</td><td>14,815</td><td>37,747</td><td>16,9</td><td>18,8</td><td>0,4</td><td>0,4</td><td>ECSV</td><td>1</td></tr><tr><td>67</td><td>15,135</td><td>37,755</td><td>69,4</td><td>-4,7</td><td>0,4</td><td>0,4</td><td>ESAL</td><td>1</td></tr><tr><td>68</td><td>14,927</td><td>37,764</td><td>13,8</td><td>17,2</td><td>0,4</td><td>0,4</td><td>EMEG</td><td>1</td></tr><tr><td>69</td><td>14,986</td><td>37,765</td><td>33,7</td><td>20,9</td><td>0,4</td><td>0,4</td><td>EPLU</td><td>1</td></tr><tr><td>70</td><td>14,846</td><td>37,789</td><td>21,3</td><td>19,1</td><td>0,8</td><td>0,5</td><td>BRON</td><td>3</td></tr><tr><td>71</td><td>15,034</td><td>37,791</td><td>52,3</td><td>29,2</td><td>0,3</td><td>0,3</td><td>EMCN</td><td>1</td></tr><tr><td>72</td><td>14,931</td><td>37,792</td><td>19,5</td><td>21,4</td><td>0,3</td><td>0,3</td><td>EMAL</td><td>1</td></tr><tr><td>73</td><td>15,177</td><td>37,821</td><td>24,6</td><td>20,8</td><td>0,3</td><td>0,3</td><td>EPMN</td><td>9</td></tr><tr><td>74</td><td>14,95</td><td>37,821</td><td>21,6</td><td>21,8</td><td>0,4</td><td>0,4</td><td>EMSG</td><td>1</td></tr><tr><td>75</td><td>15,009</td><td>37,821</td><td>22,6</td><td>25,5</td><td>0,3</td><td>0,3</td><td>EDAM</td><td>1</td></tr><tr><td>76</td><td>12,806</td><td>37,828</td><td>21,4</td><td>18</td><td>0,4</td><td>0,4</td><td>SALE</td><td>6</td></tr><tr><td>77</td><td>14,876</td><td>37,829</td><td>18,5</td><td>23,1</td><td>0,4</td><td>0,4</td><td>EPZF</td><td>1</td></tr><tr><td>78</td><td>14,713</td><td>37,848</td><td>20,5</td><td>20,5</td><td>0,4</td><td>0,4</td><td>9520</td><td>6</td></tr><tr><td>79</td><td>15,289</td><td>37,853</td><td>22,7</td><td>19,6</td><td>0,4</td><td>0,4</td><td>TAOR</td><td>6</td></tr><tr><td>80</td><td>13,193</td><td>37,864</td><td>21,9</td><td>19,7</td><td>0,8</td><td>0,8</td><td>MGAI</td><td>4</td></tr><tr><td>81</td><td>15,265</td><td>37,87</td><td>20,7</td><td>18,7</td><td>0,4</td><td>0,4</td><td>9532</td><td>6</td></tr><tr><td>82</td><td>14,907</td><td>37,889</td><td>21,3</td><td>20,7</td><td>0,3</td><td>0,3</td><td>ECAN</td><td>1</td></tr><tr><td>83</td><td>13,304</td><td>37,894</td><td>21,1</td><td>18,7</td><td>0,3</td><td>0,3</td><td>CORL</td><td>1</td></tr><tr><td>84</td><td>12,762</td><td>37,895</td><td>21,1</td><td>18,2</td><td>0,8</td><td>0,8</td><td>MGRA</td><td>4</td></tr><tr><td>85</td><td>20,702</td><td>37,931</td><td>15,2</td><td>1,9</td><td>0,3</td><td>0,3</td><td>SKIN</td><td>7</td></tr><tr><td>86</td><td>12,327</td><td>37,932</td><td>21,3</td><td>18,7</td><td>0,3</td><td>0,3</td><td>FAVI</td><td>6</td></tr><tr><td>87</td><td>15,254</td><td>37,935</td><td>23,8</td><td>21,6</td><td>0,4</td><td>0,6</td><td>MMME</td><td>8</td></tr><tr><td>88</td><td>15,005</td><td>37,951</td><td>22,1</td><td>20,4</td><td>0,4</td><td>0,4</td><td>9518</td><td>6</td></tr><tr><td>89</td><td>16,007</td><td>37,953</td><td>23,9</td><td>17,8</td><td>0,3</td><td>0,3</td><td>MPAZ</td><td>6</td></tr><tr><td>90</td><td>12,072</td><td>37,969</td><td>21,2</td><td>18,9</td><td>0,3</td><td>0,3</td><td>MARX</td><td>6</td></tr><tr><td>91</td><td>14,906</td><td>37,989</td><td>19,7</td><td>18,1</td><td>0,6</td><td>0,6</td><td>FLOR</td><td>9</td></tr><tr><td>92</td><td>14,026</td><td>37,99</td><td>22</td><td>21,1</td><td>0,3</td><td>0,4</td><td>GBLM</td><td>1</td></tr><tr><td>93</td><td>15,7</td><td>38,003</td><td>23,8</td><td>17,8</td><td>0,3</td><td>0,3</td><td>MTTG</td><td>1</td></tr><tr><td>94</td><td>12,584</td><td>38,008</td><td>21,6</td><td>18,2</td><td>0,3</td><td>0,3</td><td>MILO</td><td>6</td></tr></table>
<table><tr><td>95</td><td>15,014</td><td>38,024</td><td>22,2</td><td>21,6</td><td>0,2</td><td>0,2</td><td>MONT</td><td>9</td></tr><tr><td>96</td><td>15,136</td><td>38,029</td><td>23,7</td><td>19</td><td>0,6</td><td>0,6</td><td>NOVA</td><td>9</td></tr><tr><td>97</td><td>15,136</td><td>38,029</td><td>22</td><td>20,2</td><td>0,6</td><td>0,6</td><td>MNOV</td><td>6</td></tr><tr><td>98</td><td>21,46</td><td>38,06</td><td>9,5</td><td>-9,2</td><td>0,3</td><td>0,3</td><td>RLS0</td><td>1</td></tr><tr><td>99</td><td>15,23</td><td>38,065</td><td>24,4</td><td>20,9</td><td>0,3</td><td>0,4</td><td>MCSR</td><td>3</td></tr><tr><td>100</td><td>15,488</td><td>38,078</td><td>24,1</td><td>18,3</td><td>0,3</td><td>0,3</td><td>SPLA</td><td>6</td></tr><tr><td>101</td><td>14,919</td><td>38,1</td><td>21,2</td><td>19,4</td><td>0,6</td><td>0,6</td><td>FDNV</td><td>9</td></tr><tr><td>102</td><td>15,167</td><td>38,108</td><td>23,6</td><td>19,8</td><td>0,6</td><td>0,6</td><td>RODI</td><td>9</td></tr><tr><td>103</td><td>15,651</td><td>38,108</td><td>23,6</td><td>18,6</td><td>0,3</td><td>0,3</td><td>TGRC</td><td>6</td></tr><tr><td>104</td><td>15,036</td><td>38,138</td><td>21,6</td><td>22,3</td><td>0,3</td><td>0,3</td><td>TIND</td><td>9</td></tr><tr><td>105</td><td>15,353</td><td>38,147</td><td>24,4</td><td>18,8</td><td>0,4</td><td>0,4</td><td>MPNC</td><td>6</td></tr><tr><td>106</td><td>14,74</td><td>38,157</td><td>22,3</td><td>21,6</td><td>0,3</td><td>0,3</td><td>CAPO</td><td>9</td></tr><tr><td>107</td><td>13,314</td><td>38,162</td><td>21,7</td><td>18,8</td><td>0,5</td><td>0,5</td><td>PING</td><td>6</td></tr><tr><td>108</td><td>15,501</td><td>38,171</td><td>23,1</td><td>18,7</td><td>0,6</td><td>0,6</td><td>MM01</td><td>1</td></tr><tr><td>109</td><td>20,342</td><td>38,18</td><td>18,9</td><td>11,1</td><td>0,3</td><td>0,3</td><td>GERO</td><td>7</td></tr><tr><td>110</td><td>14,92</td><td>38,18</td><td>22,1</td><td>21,8</td><td>0,3</td><td>0,3</td><td>CALA</td><td>9</td></tr><tr><td>111</td><td>20,59</td><td>38,18</td><td>17,4</td><td>4,4</td><td>0,5</td><td>0,5</td><td>VLSM</td><td>1</td></tr><tr><td>112</td><td>15,554</td><td>38,184</td><td>23,3</td><td>17,7</td><td>0,3</td><td>0,3</td><td>MESA</td><td>6</td></tr><tr><td>113</td><td>20,35</td><td>38,2</td><td>18,4</td><td>9,5</td><td>0,8</td><td>0,8</td><td>KIPO</td><td>1</td></tr><tr><td>114</td><td>15,554</td><td>38,205</td><td>23,2</td><td>18,5</td><td>0,3</td><td>0,3</td><td>MESS</td><td>6</td></tr><tr><td>115</td><td>15,7</td><td>38,22</td><td>23,1</td><td>18,8</td><td>0,5</td><td>0,5</td><td>MM09</td><td>1</td></tr><tr><td>116</td><td>15,642</td><td>38,224</td><td>23</td><td>18,4</td><td>0,3</td><td>0,3</td><td>VLSG</td><td>6</td></tr><tr><td>117</td><td>15,646</td><td>38,226</td><td>24,2</td><td>18,9</td><td>0,5</td><td>0,5</td><td>MM11</td><td>1</td></tr><tr><td>118</td><td>15,637</td><td>38,232</td><td>22,7</td><td>18,8</td><td>0,5</td><td>0,5</td><td>MM10</td><td>1</td></tr><tr><td>119</td><td>15,711</td><td>38,233</td><td>23,9</td><td>18,1</td><td>0,3</td><td>0,3</td><td>SCRI</td><td>6</td></tr><tr><td>120</td><td>16,24</td><td>38,236</td><td>23,6</td><td>18,3</td><td>0,3</td><td>0,3</td><td>LOCR</td><td>3</td></tr><tr><td>121</td><td>15,554</td><td>38,243</td><td>24,1</td><td>18,9</td><td>0,4</td><td>0,4</td><td>AREN</td><td>6</td></tr><tr><td>122</td><td>15,684</td><td>38,244</td><td>23,7</td><td>19,2</td><td>0,5</td><td>0,5</td><td>MM08</td><td>1</td></tr><tr><td>123</td><td>15,628</td><td>38,26</td><td>23</td><td>19,8</td><td>0,9</td><td>0,9</td><td>MM06</td><td>9</td></tr><tr><td>124</td><td>15,894</td><td>38,26</td><td>23,6</td><td>17,9</td><td>0,4</td><td>0,4</td><td>CELL</td><td>6</td></tr><tr><td>125</td><td>15,508</td><td>38,264</td><td>23,2</td><td>19,2</td><td>0,3</td><td>0,3</td><td>MSRU</td><td>1</td></tr><tr><td>126</td><td>15,52</td><td>38,266</td><td>22,6</td><td>18,8</td><td>0,2</td><td>0,2</td><td>PACE</td><td>6</td></tr><tr><td>127</td><td>15,622</td><td>38,268</td><td>24,4</td><td>19</td><td>0,3</td><td>0,3</td><td>SPUR</td><td>6</td></tr><tr><td>128</td><td>15,231</td><td>38,271</td><td>23</td><td>19,6</td><td>0,3</td><td>0,3</td><td>MILA</td><td>8</td></tr><tr><td>129</td><td>21,79</td><td>38,28</td><td>6,9</td><td>-8</td><td>1,3</td><td>1,3</td><td>PAT0</td><td>6</td></tr><tr><td>130</td><td>14,985</td><td>38,378</td><td>21,7</td><td>23,7</td><td>0,3</td><td>0,3</td><td>VSER</td><td>1</td></tr><tr><td>131</td><td>14,961</td><td>38,39</td><td>21,3</td><td>24,2</td><td>0,5</td><td>0,5</td><td>VSAR</td><td>1</td></tr><tr><td>132</td><td>14,974</td><td>38,395</td><td>21,6</td><td>23,7</td><td>0,5</td><td>0,5</td><td>VROS</td><td>9</td></tr><tr><td>133</td><td>14,948</td><td>38,396</td><td>23,8</td><td>24,5</td><td>0,3</td><td>0,3</td><td>IVLT</td><td>9</td></tr><tr><td>134</td><td>14,986</td><td>38,396</td><td>21,8</td><td>23,6</td><td>0,5</td><td>0,5</td><td>VMOL</td><td>1</td></tr><tr><td>135</td><td>14,952</td><td>38,409</td><td>23,4</td><td>21,2</td><td>0,4</td><td>0,4</td><td>VCSP</td><td>6</td></tr><tr><td>136</td><td>14,952</td><td>38,417</td><td>23,3</td><td>21,8</td><td>0,3</td><td>0,3</td><td>VUCA</td><td>1</td></tr><tr><td>137</td><td>15,895</td><td>38,422</td><td>23</td><td>18,1</td><td>0,3</td><td>0,3</td><td>GIOI</td><td>7</td></tr><tr><td>138</td><td>14,963</td><td>38,426</td><td>21,8</td><td>20</td><td>0,6</td><td>0,6</td><td>VVUL</td><td>1</td></tr><tr><td>139</td><td>21,93</td><td>38,43</td><td>11,4</td><td>2,1</td><td>0,3</td><td>0,3</td><td>EYPA</td><td>6</td></tr><tr><td>140</td><td>14,956</td><td>38,43</td><td>21,6</td><td>21,1</td><td>0,5</td><td>0,5</td><td>VPLI</td><td>1</td></tr><tr><td>141</td><td>16,574</td><td>38,439</td><td>24,9</td><td>17,2</td><td>0,2</td><td>0,3</td><td>MOST</td><td>3</td></tr><tr><td>142</td><td>14,945</td><td>38,444</td><td>22,8</td><td>21,1</td><td>0,4</td><td>0,4</td><td>LFAL</td><td>1</td></tr></table>
<table><tr><td>143</td><td>16,438</td><td>38,449</td><td>23,7</td><td>18</td><td>0,3</td><td>0,3</td><td>PLAC</td><td>6</td></tr><tr><td>144</td><td>14,946</td><td>38,455</td><td>22</td><td>21,2</td><td>0,3</td><td>0,3</td><td>LGUA</td><td>1</td></tr><tr><td>145</td><td>14,905</td><td>38,483</td><td>22,8</td><td>18,5</td><td>0,5</td><td>0,5</td><td>LMAZ</td><td>1</td></tr><tr><td>146</td><td>14,356</td><td>38,534</td><td>21,2</td><td>19,5</td><td>0,3</td><td>0,3</td><td>IACL</td><td>6</td></tr><tr><td>147</td><td>14,872</td><td>38,56</td><td>24,3</td><td>16,4</td><td>0,5</td><td>0,5</td><td>SALI</td><td>1</td></tr><tr><td>148</td><td>20,543</td><td>38,564</td><td>20</td><td>10</td><td>0,5</td><td>0,5</td><td>DUKA</td><td>7</td></tr><tr><td>149</td><td>14,575</td><td>38,564</td><td>22,6</td><td>18,5</td><td>0,3</td><td>0,3</td><td>IFIL</td><td>6</td></tr><tr><td>150</td><td>15,91</td><td>38,6</td><td>24,7</td><td>19,4</td><td>0,6</td><td>0,6</td><td>PORO</td><td>1</td></tr><tr><td>151</td><td>15,886</td><td>38,607</td><td>23,7</td><td>18,2</td><td>0,3</td><td>0,3</td><td>JOPP</td><td>1</td></tr><tr><td>152</td><td>20,59</td><td>38,62</td><td>20,3</td><td>7,8</td><td>0,8</td><td>0,8</td><td>PONT</td><td>1</td></tr><tr><td>153</td><td>15,074</td><td>38,633</td><td>22,1</td><td>16,8</td><td>0,6</td><td>0,6</td><td>PANA</td><td>1</td></tr><tr><td>154</td><td>15,111</td><td>38,638</td><td>21,6</td><td>18,1</td><td>0,4</td><td>0,4</td><td>LIBI</td><td>7</td></tr><tr><td>155</td><td>15,1</td><td>38,642</td><td>21,4</td><td>17,8</td><td>0,3</td><td>0,3</td><td>PNRL</td><td>1</td></tr><tr><td>156</td><td>15,077</td><td>38,643</td><td>24</td><td>17,7</td><td>0,3</td><td>0,3</td><td>CPAN</td><td>6</td></tr><tr><td>157</td><td>15,116</td><td>38,662</td><td>22,7</td><td>16,7</td><td>1</td><td>1</td><td>BA3D</td><td>1</td></tr><tr><td>158</td><td>15,897</td><td>38,679</td><td>24,5</td><td>17,6</td><td>0,3</td><td>0,3</td><td>TRO2</td><td>3</td></tr><tr><td>159</td><td>16,547</td><td>38,684</td><td>24,4</td><td>17,5</td><td>0,3</td><td>0,3</td><td>SOV1</td><td>3</td></tr><tr><td>160</td><td>13,179</td><td>38,708</td><td>22,2</td><td>17,1</td><td>0,3</td><td>0,3</td><td>USIX</td><td>6</td></tr><tr><td>161</td><td>20,67</td><td>38,78</td><td>21,6</td><td>4,3</td><td>0,8</td><td>0,8</td><td>SPAN</td><td>1</td></tr><tr><td>162</td><td>15,241</td><td>38,801</td><td>22,2</td><td>16,6</td><td>0,6</td><td>0,6</td><td>STRO</td><td>1</td></tr><tr><td>163</td><td>21,165</td><td>38,864</td><td>16,8</td><td>10,9</td><td>0,3</td><td>0,3</td><td>AMFI</td><td>7</td></tr><tr><td>164</td><td>16,235</td><td>38,878</td><td>23,8</td><td>17,9</td><td>0,2</td><td>0,2</td><td>LAME</td><td>3</td></tr><tr><td>165</td><td>21,81</td><td>38,917</td><td>16,7</td><td>5,4</td><td>0,3</td><td>0,3</td><td>KARP</td><td>7</td></tr><tr><td>166</td><td>16,58</td><td>38,929</td><td>24,2</td><td>17,3</td><td>0,4</td><td>0,3</td><td>CAT1</td><td>3</td></tr><tr><td>167</td><td>9</td><td>39,011</td><td>22,3</td><td>15</td><td>0,2</td><td>0,3</td><td>CA02</td><td>3</td></tr><tr><td>168</td><td>16,986</td><td>39,032</td><td>24,8</td><td>17,8</td><td>0,4</td><td>0,3</td><td>CUT1</td><td>3</td></tr><tr><td>169</td><td>16,689</td><td>39,036</td><td>24,1</td><td>18</td><td>0,1</td><td>0,2</td><td>SERS</td><td>3</td></tr><tr><td>170</td><td>16,077</td><td>39,12</td><td>22,8</td><td>18,3</td><td>0,2</td><td>0,2</td><td>AMAN</td><td>3</td></tr><tr><td>171</td><td>8,973</td><td>39,136</td><td>22,5</td><td>14,6</td><td>0,2</td><td>0,2</td><td>CAGL</td><td>1</td></tr><tr><td>172</td><td>20,249</td><td>39,141</td><td>24,4</td><td>17,3</td><td>0,3</td><td>0,3</td><td>APAX</td><td>7</td></tr><tr><td>173</td><td>9,521</td><td>39,143</td><td>22,4</td><td>15,2</td><td>0,3</td><td>0,2</td><td>VILS</td><td>3</td></tr><tr><td>174</td><td>16,915</td><td>39,148</td><td>25,3</td><td>18,1</td><td>0,2</td><td>0,2</td><td>STSV</td><td>3</td></tr><tr><td>175</td><td>16,31</td><td>39,201</td><td>22,7</td><td>18,9</td><td>0,5</td><td>0,5</td><td>COSE</td><td></td></tr><tr><td>176</td><td>16,776</td><td>39,226</td><td>24,9</td><td>18,3</td><td>0,2</td><td>0,2</td><td>CCRI</td><td>3</td></tr><tr><td>177</td><td>20,128</td><td>39,236</td><td>24,5</td><td>17,2</td><td>0,3</td><td>0,3</td><td>PAXI</td><td>7</td></tr><tr><td>178</td><td>16,211</td><td>39,254</td><td>23,3</td><td>18,7</td><td>0,3</td><td>0,2</td><td>CARO</td><td>3</td></tr><tr><td>179</td><td>16,689</td><td>39,263</td><td>23,9</td><td>18,1</td><td>0,3</td><td>0,4</td><td>SANG</td><td>3</td></tr><tr><td>180</td><td>16,547</td><td>39,278</td><td>23,5</td><td>18,6</td><td>0,2</td><td>0,3</td><td>CRLM</td><td>3</td></tr><tr><td>181</td><td>16,449</td><td>39,34</td><td>24,2</td><td>18,1</td><td>0,2</td><td>0,3</td><td>CAMO</td><td>3</td></tr><tr><td>182</td><td>16,226</td><td>39,367</td><td>24,4</td><td>18,2</td><td>0,3</td><td>0,3</td><td>ARCA</td><td>3</td></tr><tr><td>183</td><td>16,226</td><td>39,431</td><td>23,7</td><td>18,6</td><td>0,3</td><td>0,2</td><td>TVRN</td><td>3</td></tr><tr><td>184</td><td>16,288</td><td>39,446</td><td>23,5</td><td>18,7</td><td>0,2</td><td>0,3</td><td>LUZZ</td><td>3</td></tr><tr><td>185</td><td>16,16</td><td>39,453</td><td>23,1</td><td>18,2</td><td>0,3</td><td>0,3</td><td>REGI</td><td>3</td></tr><tr><td>186</td><td>16,816</td><td>39,485</td><td>23,6</td><td>18,3</td><td>0,1</td><td>0,2</td><td>PIPA</td><td>3</td></tr><tr><td>187</td><td>16,287</td><td>39,513</td><td>23,1</td><td>18,6</td><td>0,2</td><td>0,2</td><td>BISI</td><td>3</td></tr><tr><td>188</td><td>15,955</td><td>39,529</td><td>23,1</td><td>18</td><td>0,2</td><td>0,2</td><td>CETR</td><td>3</td></tr><tr><td>189</td><td>16,641</td><td>39,6</td><td>24,4</td><td>19,2</td><td>0,3</td><td>0,3</td><td>ROSS</td><td>3</td></tr><tr><td>190</td><td>15,822</td><td>39,676</td><td>22,1</td><td>18,2</td><td>0,4</td><td>0,3</td><td>DIMT</td><td>3</td></tr></table>
<table><tr><td>191</td><td>9,106</td><td>39,743</td><td>22,4</td><td>14,9</td><td>0,3</td><td>0,3</td><td>ISIL</td><td>3</td></tr><tr><td>192</td><td>19,936</td><td>39,746</td><td>18,9</td><td>14,7</td><td>0,2</td><td>0,2</td><td>KASI</td><td>3</td></tr><tr><td>193</td><td>16,205</td><td>39,81</td><td>22,8</td><td>18,6</td><td>0,4</td><td>0,3</td><td>CASV</td><td>3</td></tr><tr><td>194</td><td>16,527</td><td>39,869</td><td>23,8</td><td>19</td><td>0,3</td><td>0,3</td><td>TRE2</td><td>3</td></tr><tr><td>195</td><td>16,346</td><td>39,877</td><td>23,7</td><td>19,2</td><td>0,4</td><td>0,4</td><td>SALB</td><td>3</td></tr><tr><td>196</td><td>9,548</td><td>39,883</td><td>22,2</td><td>14,6</td><td>0,3</td><td>0,2</td><td>LANU</td><td>3</td></tr><tr><td>197</td><td>15,78</td><td>39,897</td><td>21,4</td><td>17,7</td><td>0,5</td><td>0,3</td><td>PRAI</td><td>3</td></tr><tr><td>198</td><td>18,162</td><td>39,928</td><td>24,1</td><td>18,7</td><td>0,1</td><td>0,2</td><td>UGEN</td><td>3</td></tr><tr><td>199</td><td>15,816</td><td>39,994</td><td>22</td><td>18,4</td><td>0,2</td><td>0,2</td><td>CUCC</td><td>3</td></tr><tr><td>200</td><td>18,467</td><td>40,072</td><td>23,7</td><td>18,2</td><td>0,1</td><td>0,2</td><td>SCTE</td><td>3</td></tr><tr><td>201</td><td>15,63</td><td>40,074</td><td>21,9</td><td>18,1</td><td>0,3</td><td>0,4</td><td>SAPR</td><td>3</td></tr><tr><td>202</td><td>15,378</td><td>40,078</td><td>22,3</td><td>17,4</td><td>0,1</td><td>0,2</td><td>BULG</td><td>3</td></tr><tr><td>203</td><td>18,43</td><td>40,124</td><td>24,1</td><td>18,3</td><td>0,1</td><td>0,2</td><td>GIUR</td><td>3</td></tr><tr><td>204</td><td>15,866</td><td>40,184</td><td>23,7</td><td>19,2</td><td>0,2</td><td>0,2</td><td>SIRI</td><td>3</td></tr><tr><td>205</td><td>16,085</td><td>40,19</td><td>23,1</td><td>18,6</td><td>0,2</td><td>0,2</td><td>SCHR</td><td>3</td></tr><tr><td>206</td><td>15,266</td><td>40,231</td><td>22,5</td><td>17,1</td><td>0,2</td><td>0,2</td><td>VLUC</td><td>3</td></tr><tr><td>207</td><td>15,751</td><td>40,266</td><td>23,1</td><td>18,6</td><td>0,2</td><td>0,2</td><td>MTSN</td><td>3</td></tr><tr><td>208</td><td>14,941</td><td>40,269</td><td>21,9</td><td>16,7</td><td>0,3</td><td>0,4</td><td>CASY</td><td>3</td></tr><tr><td>209</td><td>15,109</td><td>40,312</td><td>23,3</td><td>15,6</td><td>0,5</td><td>1</td><td>PRIG</td><td>3</td></tr><tr><td>210</td><td>15,303</td><td>40,318</td><td>22</td><td>16,8</td><td>0,2</td><td>0,2</td><td>CMPR</td><td>3</td></tr><tr><td>211</td><td>15,802</td><td>40,325</td><td>22,8</td><td>19,2</td><td>0,2</td><td>0,2</td><td>MCEL</td><td>3</td></tr><tr><td>212</td><td>18,111</td><td>40,335</td><td>24,1</td><td>17,8</td><td>0,2</td><td>0,4</td><td>USAL</td><td>3</td></tr><tr><td>213</td><td>16,435</td><td>40,381</td><td>23,3</td><td>19,1</td><td>0,1</td><td>0,2</td><td>CRAC</td><td>3</td></tr><tr><td>214</td><td>17,965</td><td>40,385</td><td>24</td><td>18,6</td><td>0,1</td><td>0,2</td><td>SASA</td><td>3</td></tr><tr><td>215</td><td>15,633</td><td>40,391</td><td>22,1</td><td>16,9</td><td>0,4</td><td>0,3</td><td>SLCN</td><td>3</td></tr><tr><td>216</td><td>15,557</td><td>40,417</td><td>23,2</td><td>18,3</td><td>0,5</td><td>0,3</td><td>SAL1</td><td>3</td></tr><tr><td>217</td><td>15,305</td><td>40,49</td><td>21,1</td><td>16,9</td><td>0,2</td><td>0,2</td><td>CDRU</td><td>3</td></tr><tr><td>218</td><td>21,269</td><td>40,519</td><td>25</td><td>10,8</td><td>0,3</td><td>0,3</td><td>KAST</td><td>7</td></tr><tr><td>219</td><td>17,283</td><td>40,527</td><td>23,2</td><td>19,6</td><td>0,2</td><td>0,3</td><td>TARA</td><td>3</td></tr><tr><td>220</td><td>16,061</td><td>40,532</td><td>22,6</td><td>19</td><td>0,2</td><td>0,3</td><td>PTRP</td><td>3</td></tr><tr><td>221</td><td>14,987</td><td>40,547</td><td>20,8</td><td>17,3</td><td>0,3</td><td>0,4</td><td>EBOL</td><td></td></tr><tr><td>222</td><td>8,3128</td><td>40,5583</td><td>22,4</td><td>15,4</td><td>0,3</td><td>0,4</td><td>GALG</td><td></td></tr><tr><td>223</td><td>16,758</td><td>40,578</td><td>24,1</td><td>19,1</td><td>0,1</td><td>0,2</td><td>GINO</td><td>3</td></tr><tr><td>224</td><td>14,335</td><td>40,582</td><td>21,5</td><td>16,6</td><td>0,1</td><td>0,1</td><td>ENAV</td><td>1</td></tr><tr><td>225</td><td>15,724</td><td>40,601</td><td>22,6</td><td>19,6</td><td>0,1</td><td>0,2</td><td>TITO</td><td>3</td></tr><tr><td>226</td><td>16,441</td><td>40,604</td><td>23</td><td>18,9</td><td>0,1</td><td>0,2</td><td>SVTO</td><td>3</td></tr><tr><td>227</td><td>14,374</td><td>40,626</td><td>21,3</td><td>16,8</td><td>0,2</td><td>0,4</td><td>SORR</td><td></td></tr><tr><td>228</td><td>16,704</td><td>40,649</td><td>23</td><td>19,3</td><td>0,1</td><td>0,1</td><td>MATE</td><td>11</td></tr><tr><td>229</td><td>15,851</td><td>40,658</td><td>23,3</td><td>19,5</td><td>0,2</td><td>0,2</td><td>CAMA</td><td>3</td></tr><tr><td>230</td><td>19,945</td><td>40,708</td><td>21,2</td><td>15,1</td><td>0,3</td><td>0,2</td><td>BERA</td><td>3</td></tr><tr><td>231</td><td>8,5673</td><td>40,7211</td><td>22,4</td><td>15,1</td><td>0,6</td><td>0,8</td><td>SASS</td><td>3</td></tr><tr><td>232</td><td>15,489</td><td>40,756</td><td>23,9</td><td>19,5</td><td>0,2</td><td>0,3</td><td>MRLC</td><td>3</td></tr><tr><td>233</td><td>15,168</td><td>40,783</td><td>22,1</td><td>17,6</td><td>0,3</td><td>0,3</td><td>MCRV</td><td>3</td></tr><tr><td>234</td><td>15,942</td><td>40,787</td><td>22,9</td><td>19,1</td><td>0,2</td><td>0,3</td><td>ACER</td><td>3</td></tr><tr><td>235</td><td>17,064</td><td>40,789</td><td>24,1</td><td>18,9</td><td>0,1</td><td>0,2</td><td>NOCI</td><td>3</td></tr><tr><td>236</td><td>13,422</td><td>40,795</td><td>20,9</td><td>16,7</td><td>0,1</td><td>0,2</td><td>VENT</td><td>3</td></tr><tr><td>237</td><td>17,359</td><td>40,835</td><td>24,3</td><td>19</td><td>0,2</td><td>0,2</td><td>FASA</td><td>3</td></tr><tr><td>238</td><td>15,022</td><td>40,844</td><td>21,7</td><td>16,9</td><td>0,4</td><td>0,4</td><td>AV02</td><td>3</td></tr></table>
<table><tr><td>239</td><td>14,556</td><td>40,87</td><td>21</td><td>17</td><td>0,1</td><td>0,2</td><td>PACA</td><td></td></tr><tr><td>240</td><td>14,63</td><td>40,874</td><td>20,3</td><td>17,6</td><td>0,4</td><td>0,6</td><td>AV03</td><td>3</td></tr><tr><td>241</td><td>15,439</td><td>40,9</td><td>22,9</td><td>19,1</td><td>0,2</td><td>0,4</td><td>AV04</td><td>3</td></tr><tr><td>242</td><td>16,604</td><td>40,907</td><td>23,1</td><td>19,2</td><td>0,1</td><td>0,2</td><td>AMUR</td><td>3</td></tr><tr><td>243</td><td>9,1</td><td>40,908</td><td>22,6</td><td>15,4</td><td>0,2</td><td>0,1</td><td>TEMP</td><td>3</td></tr><tr><td>244</td><td>14,783</td><td>40,912</td><td>21,6</td><td>18,3</td><td>0,3</td><td>0,3</td><td>AVEL</td><td>3</td></tr><tr><td>245</td><td>16,254</td><td>40,917</td><td>23,8</td><td>19,2</td><td>0,1</td><td>0,2</td><td>POGG</td><td>3</td></tr><tr><td>246</td><td>15,209</td><td>40,925</td><td>22,3</td><td>17,8</td><td>0,1</td><td>0,2</td><td>SNAL</td><td>3</td></tr><tr><td>247</td><td>15,184</td><td>40,931</td><td>21,3</td><td>18,1</td><td>0,2</td><td>0,3</td><td>ANGE</td><td>3</td></tr><tr><td>248</td><td>9,497</td><td>40,941</td><td>22,8</td><td>15,7</td><td>0,4</td><td>0,5</td><td>OLBI</td><td>3</td></tr><tr><td>249</td><td>15,96</td><td>40,944</td><td>22,9</td><td>19,1</td><td>0,1</td><td>0,2</td><td>PALZ</td><td>3</td></tr><tr><td>250</td><td>15,616</td><td>40,955</td><td>23,2</td><td>19,1</td><td>0,1</td><td>0,2</td><td>VULT</td><td>3</td></tr><tr><td>251</td><td>15,809</td><td>40,967</td><td>23,9</td><td>19,5</td><td>0,3</td><td>0,6</td><td>VENO</td><td>3</td></tr><tr><td>252</td><td>16,904</td><td>41,016</td><td>24,2</td><td>19,4</td><td>0,2</td><td>0,2</td><td>VALI</td><td>3</td></tr><tr><td>253</td><td>21,335</td><td>41,024</td><td>23,8</td><td>11,4</td><td>0,3</td><td>0,4</td><td>BITO</td><td>3</td></tr><tr><td>254</td><td>15,237</td><td>41,028</td><td>22</td><td>18,3</td><td>0,1</td><td>0,2</td><td>CAFE</td><td>3</td></tr><tr><td>255</td><td>14,568</td><td>41,031</td><td>21,1</td><td>16,8</td><td>0,4</td><td>0,4</td><td>PAOL</td><td>3</td></tr><tr><td>256</td><td>14,327</td><td>41,047</td><td>21,5</td><td>18,3</td><td>0,2</td><td>0,3</td><td>NICY</td><td></td></tr><tr><td>257</td><td>16,196</td><td>41,061</td><td>23</td><td>19,2</td><td>0,1</td><td>0,2</td><td>MRVN</td><td>3</td></tr><tr><td>258</td><td>15,101</td><td>41,067</td><td>21,6</td><td>17,4</td><td>0,2</td><td>0,3</td><td>GRO1</td><td>3</td></tr><tr><td>259</td><td>15,06</td><td>41,073</td><td>21,8</td><td>17,6</td><td>0,1</td><td>0,2</td><td>GROT</td><td>3</td></tr><tr><td>260</td><td>16,274</td><td>41,078</td><td>23,1</td><td>19,2</td><td>0,1</td><td>0,1</td><td>CADM</td><td>3</td></tr><tr><td>261</td><td>15,083</td><td>41,11</td><td>22</td><td>17,6</td><td>0,2</td><td>0,3</td><td>AV01</td><td>3</td></tr><tr><td>262</td><td>20,794</td><td>41,127</td><td>23,4</td><td>12,5</td><td>0,2</td><td>0,2</td><td>OHRI</td><td>3</td></tr><tr><td>263</td><td>15,365</td><td>41,136</td><td>22,7</td><td>18,9</td><td>0,2</td><td>0,2</td><td>SGTA</td><td>3</td></tr><tr><td>264</td><td>13,881</td><td>41,146</td><td>20,6</td><td>16,8</td><td>0,1</td><td>0,2</td><td>MODR</td><td>3</td></tr><tr><td>265</td><td>15,331</td><td>41,159</td><td>23,7</td><td>19,1</td><td>0,2</td><td>0,3</td><td>ACCA</td><td>3</td></tr><tr><td>266</td><td>13,974</td><td>41,195</td><td>20,2</td><td>17,3</td><td>0,3</td><td>0,4</td><td>CARI</td><td>3</td></tr><tr><td>267</td><td>16,604</td><td>41,196</td><td>23,1</td><td>18,9</td><td>0,3</td><td>0,3</td><td>MLFT</td><td>3</td></tr><tr><td>268</td><td>14,811</td><td>41,223</td><td>21,9</td><td>17,5</td><td>0,1</td><td>0,2</td><td>PSB1</td><td>3</td></tr><tr><td>269</td><td>13,1</td><td>41,25</td><td>21</td><td>16,4</td><td>0,2</td><td>0,3</td><td>SFCI</td><td>3</td></tr><tr><td>270</td><td>13,699</td><td>41,281</td><td>21,6</td><td>15,6</td><td>0,3</td><td>0,3</td><td>FORM</td><td>3</td></tr><tr><td>271</td><td>14,335</td><td>41,327</td><td>21,9</td><td>17,6</td><td>0,2</td><td>0,3</td><td>ALIF</td><td>3</td></tr><tr><td>272</td><td>21,56</td><td>41,344</td><td>23,6</td><td>11,8</td><td>0,3</td><td>0,3</td><td>PRIL</td><td>3</td></tr><tr><td>273</td><td>14,529</td><td>41,364</td><td>22,2</td><td>17,4</td><td>0,2</td><td>0,3</td><td>PTRJ</td><td>3</td></tr><tr><td>274</td><td>15,159</td><td>41,371</td><td>22,5</td><td>18,6</td><td>0,2</td><td>0,2</td><td>MOCO</td><td>3</td></tr><tr><td>275</td><td>16,149</td><td>41,373</td><td>23,7</td><td>19,2</td><td>0,1</td><td>0,2</td><td>MARG</td><td>3</td></tr><tr><td>276</td><td>14,706</td><td>41,398</td><td>21,3</td><td>17,5</td><td>0,2</td><td>0,3</td><td>SACR</td><td>3</td></tr><tr><td>277</td><td>13,765</td><td>41,407</td><td>21,1</td><td>15,9</td><td>0,2</td><td>0,4</td><td>SGLI</td><td>3</td></tr><tr><td>278</td><td>15,017</td><td>41,409</td><td>23,1</td><td>19,3</td><td>0,3</td><td>0,4</td><td>BART</td><td></td></tr><tr><td>279</td><td>14,234</td><td>41,415</td><td>21,7</td><td>17,4</td><td>0,3</td><td>0,6</td><td>VAGA</td><td>3</td></tr><tr><td>280</td><td>15,532</td><td>41,452</td><td>23,4</td><td>19</td><td>0,2</td><td>0,2</td><td>FOGG</td><td>3</td></tr><tr><td>281</td><td>12,901</td><td>41,471</td><td>21,8</td><td>16,1</td><td>0,2</td><td>0,2</td><td>LATI</td><td>3</td></tr><tr><td>282</td><td>14,253</td><td>41,501</td><td>22,2</td><td>18,2</td><td>0,2</td><td>0,4</td><td>LNGN</td><td>3</td></tr><tr><td>283</td><td>20,959</td><td>41,509</td><td>24,3</td><td>12</td><td>0,4</td><td>0,3</td><td>KICE</td><td>3</td></tr><tr><td>284</td><td>14,91</td><td>41,513</td><td>23,1</td><td>18,5</td><td>0,2</td><td>0,4</td><td>GATE</td><td>3</td></tr><tr><td>285</td><td>20,528</td><td>41,521</td><td>22,5</td><td>14,7</td><td>0,3</td><td>0,5</td><td>DEBA</td><td>3</td></tr><tr><td>286</td><td>14,594</td><td>41,546</td><td>22,6</td><td>18,2</td><td>0,1</td><td>0,2</td><td>BSSO</td><td>3</td></tr></table>
<table><tr><td>287</td><td>14,678</td><td>41,56</td><td>23,8</td><td>18</td><td>0,2</td><td>0,2</td><td>CABA</td><td>3</td></tr><tr><td>288</td><td>14,236</td><td>41,599</td><td>21,9</td><td>19,2</td><td>0,2</td><td>0,4</td><td>ISER</td><td>3</td></tr><tr><td>289</td><td>20,44</td><td>41,685</td><td>22,4</td><td>13,4</td><td>0,2</td><td>0,3</td><td>PESH</td><td>3</td></tr><tr><td>290</td><td>14,152</td><td>41,703</td><td>22,5</td><td>17,7</td><td>0,2</td><td>0,1</td><td>RNI2</td><td>3</td></tr><tr><td>291</td><td>15,127</td><td>41,706</td><td>22,8</td><td>18,4</td><td>0,2</td><td>0,4</td><td>MELA</td><td>3</td></tr><tr><td>292</td><td>15,91</td><td>41,712</td><td>23,1</td><td>18,6</td><td>0,1</td><td>0,2</td><td>MSAG</td><td>3</td></tr><tr><td>293</td><td>13,712</td><td>41,717</td><td>22,2</td><td>17,1</td><td>0,2</td><td>0,3</td><td>POFI</td><td>3</td></tr><tr><td>294</td><td>21,771</td><td>41,718</td><td>23,3</td><td>11,9</td><td>0,2</td><td>0,3</td><td>VELE</td><td>3</td></tr><tr><td>295</td><td>15,259</td><td>41,74</td><td>23,7</td><td>18,4</td><td>0,2</td><td>0,2</td><td>SPCI</td><td>3</td></tr><tr><td>296</td><td>15,744</td><td>41,755</td><td>23,4</td><td>19,3</td><td>0,1</td><td>0,3</td><td>SGRT</td><td>3</td></tr><tr><td>297</td><td>14,55</td><td>41,767</td><td>23,7</td><td>18,4</td><td>0,2</td><td>0,2</td><td>TRIV</td><td>3</td></tr><tr><td>298</td><td>13,312</td><td>41,794</td><td>22</td><td>16,6</td><td>0,2</td><td>0,2</td><td>GUAR</td><td>3</td></tr><tr><td>299</td><td>14,922</td><td>41,81</td><td>23,3</td><td>18,8</td><td>0,2</td><td>0,2</td><td>LARI</td><td>3</td></tr><tr><td>300</td><td>12,703</td><td>41,811</td><td>21,8</td><td>16,6</td><td>0,2</td><td>0,2</td><td>RMPO</td><td>3</td></tr><tr><td>301</td><td>12,515</td><td>41,828</td><td>21,6</td><td>16,4</td><td>0,1</td><td>0,1</td><td>INGR</td><td>3</td></tr><tr><td>302</td><td>9,403</td><td>41,858</td><td>22,4</td><td>15,3</td><td>0,3</td><td>0,3</td><td>SARI</td><td>3</td></tr><tr><td>303</td><td>13,623</td><td>41,87</td><td>22,3</td><td>17,4</td><td>0,2</td><td>0,3</td><td>VVLO</td><td>3</td></tr><tr><td>304</td><td>12,493</td><td>41,893</td><td>21,8</td><td>16,3</td><td>0,1</td><td>0,1</td><td>M0SE</td><td>3</td></tr><tr><td>305</td><td>15,961</td><td>41,893</td><td>23,7</td><td>19</td><td>0,3</td><td>0,4</td><td>VGAR</td><td>3</td></tr><tr><td>306</td><td>15,897</td><td>41,904</td><td>23,9</td><td>19,2</td><td>0,1</td><td>0,2</td><td>ISCH</td><td>3</td></tr><tr><td>307</td><td>12,422</td><td>41,905</td><td>21,5</td><td>16,2</td><td>0,2</td><td>0,2</td><td>ROMA</td><td>3</td></tr><tr><td>308</td><td>8,763</td><td>41,927</td><td>22,5</td><td>15,2</td><td>0,1</td><td>0,1</td><td>AJAC</td><td>3</td></tr><tr><td>309</td><td>12,982</td><td>41,949</td><td>21,6</td><td>16,3</td><td>0,2</td><td>0,2</td><td>CERT</td><td>3</td></tr><tr><td>310</td><td>14,669</td><td>41,974</td><td>23,5</td><td>18,2</td><td>0,1</td><td>0,2</td><td>FRES</td><td>3</td></tr><tr><td>311</td><td>21,407</td><td>42</td><td>23</td><td>12,4</td><td>0,2</td><td>0,3</td><td>SKOP</td><td>3</td></tr><tr><td>312</td><td>20,97</td><td>42,009</td><td>23,6</td><td>12,7</td><td>0,4</td><td>0,4</td><td>TETO</td><td>3</td></tr><tr><td>313</td><td>14,183</td><td>42,047</td><td>24,8</td><td>18,3</td><td>0,4</td><td>0,3</td><td>LPEL</td><td>3</td></tr><tr><td>314</td><td>13,924</td><td>42,048</td><td>23,7</td><td>19,2</td><td>0,2</td><td>0,3</td><td>SMRA</td><td>3</td></tr><tr><td>315</td><td>13,039</td><td>42,05</td><td>21,4</td><td>16,9</td><td>0,4</td><td>0,4</td><td>OCRA</td><td>3</td></tr><tr><td>316</td><td>19,496</td><td>42,051</td><td>22</td><td>16</td><td>0,2</td><td>0,2</td><td>SHKO</td><td>3</td></tr><tr><td>317</td><td>12,619</td><td>42,053</td><td>21</td><td>16,2</td><td>0,2</td><td>0,2</td><td>MORO</td><td>3</td></tr><tr><td>318</td><td>12,355</td><td>42,055</td><td>21,2</td><td>16,3</td><td>0,2</td><td>0,2</td><td>I</td><td>3</td></tr><tr><td>319</td><td>12</td><td>42,064</td><td>21,2</td><td>16,1</td><td>0,2</td><td>0,1</td><td>TOLF</td><td>3</td></tr><tr><td>320</td><td>11,789</td><td>42,096</td><td>21,3</td><td>15,6</td><td>0,2</td><td>0,2</td><td>CIV1</td><td>3</td></tr><tr><td>321</td><td>14,708</td><td>42,11</td><td>23,9</td><td>18,1</td><td>0,2</td><td>0,2</td><td>VTRA</td><td>3</td></tr><tr><td>322</td><td>14,228</td><td>42,124</td><td>23,8</td><td>19,3</td><td>0,2</td><td>0,2</td><td>PBRA</td><td>3</td></tr><tr><td>323</td><td>21,718</td><td>42,136</td><td>23,1</td><td>12,7</td><td>0,2</td><td>0,4</td><td>KUMA</td><td>3</td></tr><tr><td>324</td><td>13,515</td><td>42,138</td><td>22,6</td><td>18,2</td><td>0,4</td><td>0,6</td><td>OVRA</td><td>3</td></tr><tr><td>325</td><td>9,336</td><td>42,168</td><td>22,6</td><td>15</td><td>0,1</td><td>0,2</td><td>ATST</td><td>3</td></tr><tr><td>326</td><td>11,758</td><td>42,254</td><td>21,2</td><td>15,5</td><td>0,2</td><td>0,3</td><td>TARQ</td><td>3</td></tr><tr><td>327</td><td>14,002</td><td>42,268</td><td>23,8</td><td>18,4</td><td>0,2</td><td>0,2</td><td>SCRA</td><td>3</td></tr><tr><td>328</td><td>13,72</td><td>42,367</td><td>24,6</td><td>18,6</td><td>0,5</td><td>0,5</td><td>CDRA</td><td>3</td></tr><tr><td>329</td><td>13,35</td><td>42,368</td><td>22,5</td><td>16,8</td><td>0,2</td><td>0,2</td><td>AQUI</td><td>3</td></tr><tr><td>330</td><td>13,316</td><td>42,382</td><td>23,2</td><td>17,9</td><td>0,3</td><td>0,3</td><td>INGP</td><td>3</td></tr><tr><td>331</td><td>9,531</td><td>42,386</td><td>22,6</td><td>15,2</td><td>0,1</td><td>0,1</td><td>LUCI</td><td>3</td></tr><tr><td>332</td><td>12,857</td><td>42,408</td><td>21,7</td><td>16,1</td><td>0,2</td><td>0,2</td><td>RIET</td><td>3</td></tr><tr><td>333</td><td>12,119</td><td>42,418</td><td>21,1</td><td>16,5</td><td>0,4</td><td>0,4</td><td>VITE</td><td>3</td></tr><tr><td>334</td><td>14,292</td><td>42,418</td><td>23,7</td><td>18,2</td><td>0,2</td><td>0,3</td><td>FRRA</td><td>3</td></tr></table>
<table><tr><td>335</td><td>13,516</td><td>42,421</td><td>24,2</td><td>18,7</td><td>0,3</td><td>0,3</td><td>INFN</td><td>3</td></tr><tr><td>336</td><td>12,103</td><td>42,426</td><td>21,7</td><td>16,1</td><td>0,2</td><td>0,2</td><td>VITI</td><td>3</td></tr><tr><td>337</td><td>11,12</td><td>42,428</td><td>21,8</td><td>15,6</td><td>0,2</td><td>0,1</td><td>PSTE</td><td>3</td></tr><tr><td>338</td><td>11,131</td><td>42,428</td><td>21,8</td><td>15,5</td><td>0,1</td><td>0,2</td><td>MAON</td><td>3</td></tr><tr><td>339</td><td>13,208</td><td>42,445</td><td>22,2</td><td>16,9</td><td>0,2</td><td>0,2</td><td>TERM</td><td>3</td></tr><tr><td>340</td><td>12,993</td><td>42,456</td><td>22</td><td>16,6</td><td>0,5</td><td>0,4</td><td>MTTO</td><td>3</td></tr><tr><td>341</td><td>21,766</td><td>42,46</td><td>23</td><td>12,5</td><td>0,2</td><td>0,2</td><td>BUJA</td><td>3</td></tr><tr><td>342</td><td>14,139</td><td>42,519</td><td>24,2</td><td>18,4</td><td>0,3</td><td>0,3</td><td>PSAN</td><td>3</td></tr><tr><td>343</td><td>13,24</td><td>42,528</td><td>23</td><td>18,2</td><td>0,3</td><td>0,5</td><td>MTRA</td><td>3</td></tr><tr><td>344</td><td>13,409</td><td>42,529</td><td>23,3</td><td>17,7</td><td>0,2</td><td>0,3</td><td>CATO</td><td>3</td></tr><tr><td>345</td><td>14,007</td><td>42,551</td><td>24,1</td><td>18,4</td><td>0,3</td><td>0,3</td><td>ATRA</td><td>3</td></tr><tr><td>346</td><td>12,412</td><td>42,559</td><td>21,8</td><td>16,5</td><td>0,2</td><td>0,2</td><td>REAM</td><td>3</td></tr><tr><td>347</td><td>12,674</td><td>42,559</td><td>21,3</td><td>16,4</td><td>0,2</td><td>0,4</td><td>UNTR</td><td>3</td></tr><tr><td>348</td><td>12,65</td><td>42,567</td><td>21,7</td><td>16,8</td><td>0,3</td><td>0,2</td><td>TERI</td><td>3</td></tr><tr><td>349</td><td>13,04</td><td>42,603</td><td>22,3</td><td>17</td><td>0,2</td><td>0,2</td><td>LNSS</td><td>3</td></tr><tr><td>350</td><td>11,673</td><td>42,634</td><td>21,5</td><td>15,6</td><td>0,4</td><td>0,5</td><td>PITI</td><td>3</td></tr><tr><td>351</td><td>18,11</td><td>42,65</td><td>22,9</td><td>18,6</td><td>0,7</td><td>0,5</td><td>DUBR</td><td>3</td></tr><tr><td>352</td><td>13,698</td><td>42,657</td><td>23,9</td><td>18,1</td><td>0,3</td><td>0,3</td><td>TERA</td><td>3</td></tr><tr><td>353</td><td>14,001</td><td>42,658</td><td>23,7</td><td>18,1</td><td>0,1</td><td>0,1</td><td>RSTO</td><td>3</td></tr><tr><td>354</td><td>14,002</td><td>42,658</td><td>24</td><td>18,3</td><td>0,2</td><td>0,2</td><td>ITRA</td><td>3</td></tr><tr><td>355</td><td>13,498</td><td>42,735</td><td>24,2</td><td>18,9</td><td>0,3</td><td>0,3</td><td>VCRA</td><td>3</td></tr><tr><td>356</td><td>10,211</td><td>42,753</td><td>22</td><td>15,4</td><td>0,1</td><td>0,1</td><td>ELBA</td><td>3</td></tr><tr><td>357</td><td>9,475</td><td>42,775</td><td>22,4</td><td>15,2</td><td>0,3</td><td>0,4</td><td>BRDO</td><td>3</td></tr><tr><td>358</td><td>12,408</td><td>42,781</td><td>21,5</td><td>17,4</td><td>0,5</td><td>0,4</td><td>TODI</td><td>3</td></tr><tr><td>359</td><td>11,109</td><td>42,782</td><td>22</td><td>15,7</td><td>0,5</td><td>0,4</td><td>GROA</td><td>3</td></tr><tr><td>360</td><td>12,407</td><td>42,782</td><td>22,1</td><td>16,9</td><td>0,1</td><td>0,1</td><td>RETO</td><td>3</td></tr><tr><td>361</td><td>12,41</td><td>42,788</td><td>21,3</td><td>16,7</td><td>0,3</td><td>0,2</td><td>TOD2</td><td>3</td></tr><tr><td>362</td><td>10,865</td><td>42,791</td><td>21,8</td><td>15,9</td><td>0,2</td><td>0,3</td><td>CASP</td><td>3</td></tr><tr><td>363</td><td>10,295</td><td>42,793</td><td>21,4</td><td>16,1</td><td>0,3</td><td>0,2</td><td>PFER</td><td>3</td></tr><tr><td>364</td><td>13,093</td><td>42,793</td><td>22,9</td><td>17,8</td><td>0,1</td><td>0,2</td><td>RENO</td><td>3</td></tr><tr><td>365</td><td>13,637</td><td>42,822</td><td>23,8</td><td>18,2</td><td>0,2</td><td>0,3</td><td>ASCO</td><td>3</td></tr><tr><td>366</td><td>13,593</td><td>42,857</td><td>24,3</td><td>18,2</td><td>0,2</td><td>0,3</td><td>ASCC</td><td>3</td></tr><tr><td>367</td><td>13,916</td><td>42,885</td><td>24,2</td><td>18,7</td><td>0,2</td><td>0,2</td><td>MRRA</td><td>3</td></tr><tr><td>368</td><td>9,476</td><td>42,888</td><td>22,4</td><td>15,7</td><td>0,2</td><td>0,3</td><td>LURI</td><td>3</td></tr><tr><td>369</td><td>12,111</td><td>42,913</td><td>21,6</td><td>16,5</td><td>0,2</td><td>0,2</td><td>MGAB</td><td>3</td></tr><tr><td>370</td><td>10,889</td><td>42,937</td><td>21,8</td><td>16,1</td><td>0,2</td><td>0,3</td><td>CAVO</td><td>3</td></tr><tr><td>371</td><td>12,002</td><td>42,952</td><td>22</td><td>17</td><td>0,1</td><td>0,1</td><td>REPI</td><td>3</td></tr><tr><td>372</td><td>12,699</td><td>42,955</td><td>21,9</td><td>17</td><td>0,2</td><td>0,2</td><td>FOL1</td><td>3</td></tr><tr><td>373</td><td>12,704</td><td>42,956</td><td>22,2</td><td>16,7</td><td>0,2</td><td>0,1</td><td>REFO</td><td>3</td></tr><tr><td>374</td><td>13,871</td><td>42,976</td><td>25</td><td>18,7</td><td>0,2</td><td>0,3</td><td>GRAM</td><td>3</td></tr><tr><td>375</td><td>21,948</td><td>42,998</td><td>22,8</td><td>13,2</td><td>0,2</td><td>0,2</td><td>LESK</td><td>3</td></tr><tr><td>376</td><td>12,905</td><td>43,005</td><td>22,6</td><td>17,9</td><td>0,2</td><td>0,3</td><td>CESI</td><td>3</td></tr><tr><td>377</td><td>13,335</td><td>43,063</td><td>24,2</td><td>18,5</td><td>0,2</td><td>0,2</td><td>GUMA</td><td>3</td></tr><tr><td>378</td><td>12,394</td><td>43,111</td><td>22,2</td><td>17</td><td>0,2</td><td>0,2</td><td>PERU</td><td>3</td></tr><tr><td>379</td><td>13,124</td><td>43,112</td><td>24,1</td><td>18</td><td>0,3</td><td>0,4</td><td>CAME</td><td>3</td></tr><tr><td>380</td><td>12,356</td><td>43,119</td><td>22,6</td><td>16,5</td><td>0,1</td><td>0,1</td><td>UNPG</td><td>3</td></tr><tr><td>381</td><td>21,271</td><td>43,138</td><td>23,7</td><td>13,5</td><td>0,2</td><td>0,3</td><td>KURS</td><td>3</td></tr><tr><td>382</td><td>20,519</td><td>43,14</td><td>23,1</td><td>14,3</td><td>0,3</td><td>0,3</td><td>NPAZ</td><td>3</td></tr></table>
<table><tr><td>383</td><td>13,731</td><td>43,168</td><td>23,8</td><td>18,5</td><td>0,3</td><td>0,3</td><td>FRMO</td><td>3</td></tr><tr><td>384</td><td>12,351</td><td>43,2</td><td>22</td><td>16,4</td><td>0,5</td><td>0,4</td><td>ATTE</td><td>3</td></tr><tr><td>385</td><td>12,245</td><td>43,209</td><td>22,5</td><td>16,7</td><td>0,1</td><td>0,1</td><td>CSSB</td><td>3</td></tr><tr><td>386</td><td>12,782</td><td>43,234</td><td>23,9</td><td>17,6</td><td>0,3</td><td>0,2</td><td>ITGT</td><td>3</td></tr><tr><td>387</td><td>11,978</td><td>43,259</td><td>22,2</td><td>16,8</td><td>0,2</td><td>0,3</td><td>CAMU</td><td>3</td></tr><tr><td>388</td><td>12,285</td><td>43,279</td><td>22,2</td><td>16,8</td><td>0,1</td><td>0,1</td><td>VALC</td><td>3</td></tr><tr><td>389</td><td>13,451</td><td>43,294</td><td>24,3</td><td>18,5</td><td>0,1</td><td>0,1</td><td>MACE</td><td>3</td></tr><tr><td>390</td><td>10,527</td><td>43,311</td><td>22,3</td><td>15,1</td><td>0,3</td><td>0,4</td><td>CECI</td><td>3</td></tr><tr><td>391</td><td>12,329</td><td>43,311</td><td>22,4</td><td>16,4</td><td>0,2</td><td>0,3</td><td>UMBE</td><td>3</td></tr><tr><td>392</td><td>11,338</td><td>43,315</td><td>21,9</td><td>16,3</td><td>0,2</td><td>0,2</td><td>S1EN</td><td>3</td></tr><tr><td>393</td><td>12,407</td><td>43,315</td><td>22</td><td>16,5</td><td>0,2</td><td>0,2</td><td>ATLO</td><td>3</td></tr><tr><td>394</td><td>11,966</td><td>43,329</td><td>22,2</td><td>16,7</td><td>0,3</td><td>0,4</td><td>CAFI</td><td>3</td></tr><tr><td>395</td><td>12,926</td><td>43,344</td><td>23,2</td><td>18,2</td><td>0,2</td><td>0,2</td><td>ITFA</td><td>3</td></tr><tr><td>396</td><td>12,582</td><td>43,352</td><td>22,8</td><td>17,6</td><td>0,3</td><td>0,3</td><td>REGU</td><td>3</td></tr><tr><td>397</td><td>12,407</td><td>43,382</td><td>22,4</td><td>16,8</td><td>0,1</td><td>0,1</td><td>MVAL</td><td>3</td></tr><tr><td>398</td><td>19,642</td><td>43,386</td><td>22,7</td><td>15,8</td><td>0,2</td><td>0,2</td><td>PRIJ</td><td>3</td></tr><tr><td>399</td><td>9,892</td><td>43,426</td><td>22,5</td><td>15,4</td><td>0,1</td><td>0,1</td><td>GROG</td><td>3</td></tr><tr><td>400</td><td>12,402</td><td>43,451</td><td>22,6</td><td>17,1</td><td>0,1</td><td>0,1</td><td>PIET</td><td>3</td></tr><tr><td>401</td><td>12,226</td><td>43,452</td><td>24,4</td><td>18</td><td>0,2</td><td>0,2</td><td>REMO</td><td>3</td></tr><tr><td>402</td><td>11,875</td><td>43,464</td><td>23</td><td>16,9</td><td>0,1</td><td>0,1</td><td>AREZ</td><td>3</td></tr><tr><td>403</td><td>13,544</td><td>43,464</td><td>24,1</td><td>18,5</td><td>0,2</td><td>0,2</td><td>CASF</td><td>3</td></tr><tr><td>404</td><td>12,248</td><td>43,467</td><td>22,7</td><td>16,8</td><td>0,2</td><td>0,2</td><td>CIT1</td><td>3</td></tr><tr><td>405</td><td>12,548</td><td>43,476</td><td>23,3</td><td>18,5</td><td>0,6</td><td>0,4</td><td>ATBU</td><td>3</td></tr><tr><td>406</td><td>13,123</td><td>43,503</td><td>23,7</td><td>18,3</td><td>0,1</td><td>0,2</td><td>MOIE</td><td>3</td></tr><tr><td>407</td><td>16,438</td><td>43,507</td><td>23,5</td><td>18,4</td><td>0,2</td><td>0,2</td><td>SPLT</td><td>3</td></tr><tr><td>408</td><td>21,329</td><td>43,58</td><td>23,1</td><td>13,6</td><td>0,3</td><td>0,3</td><td>KRUS</td><td>3</td></tr><tr><td>409</td><td>20,23</td><td>43,581</td><td>23,3</td><td>15,3</td><td>0,2</td><td>0,3</td><td>IVAN</td><td>3</td></tr><tr><td>410</td><td>11,474</td><td>43,619</td><td>22,5</td><td>16,9</td><td>0,2</td><td>0,2</td><td>FIGL</td><td>3</td></tr><tr><td>411</td><td>12,807</td><td>43,689</td><td>23,8</td><td>18,5</td><td>0,2</td><td>0,2</td><td>FOSS</td><td>3</td></tr><tr><td>412</td><td>10,935</td><td>43,715</td><td>22,4</td><td>15,7</td><td>0,1</td><td>0,2</td><td>EMPO</td><td>3</td></tr><tr><td>413</td><td>10,366</td><td>43,747</td><td>22,9</td><td>15,8</td><td>0,2</td><td>0,2</td><td>MADA</td><td>3</td></tr><tr><td>414</td><td>11,227</td><td>43,785</td><td>22,6</td><td>17</td><td>0,3</td><td>0,3</td><td>FIPR</td><td>3</td></tr><tr><td>415</td><td>10,98</td><td>43,796</td><td>23,4</td><td>16,6</td><td>0,2</td><td>0,1</td><td>CRMI</td><td>3</td></tr><tr><td>416</td><td>11,214</td><td>43,796</td><td>22,6</td><td>17,3</td><td>0,1</td><td>0,2</td><td>IGMI</td><td>3</td></tr><tr><td>417</td><td>12,265</td><td>43,817</td><td>23,6</td><td>17,9</td><td>0,4</td><td>0,4</td><td>PEN2</td><td>3</td></tr><tr><td>418</td><td>11,164</td><td>43,868</td><td>23</td><td>17</td><td>0,2</td><td>0,2</td><td>CALA</td><td>3</td></tr><tr><td>419</td><td>18,414</td><td>43,868</td><td>23,1</td><td>16,4</td><td>0,2</td><td>0,2</td><td>SRJV</td><td>3</td></tr><tr><td>420</td><td>11,099</td><td>43,886</td><td>23</td><td>16,8</td><td>0,1</td><td>0,1</td><td>PRAT</td><td>3</td></tr><tr><td>421</td><td>12,893</td><td>43,893</td><td>23,3</td><td>18,4</td><td>0,2</td><td>0,3</td><td>PES2</td><td>3</td></tr><tr><td>422</td><td>12,451</td><td>43,933</td><td>23,8</td><td>18,2</td><td>0,1</td><td>0,2</td><td>RSMN</td><td>3</td></tr><tr><td>423</td><td>19,571</td><td>43,968</td><td>23,1</td><td>15,7</td><td>0,3</td><td>0,4</td><td>BAJI</td><td>3</td></tr><tr><td>424</td><td>10,544</td><td>43,979</td><td>22,7</td><td>16,5</td><td>0,6</td><td>0,4</td><td>MOZZ</td><td>3</td></tr><tr><td>425</td><td>20,46</td><td>44,025</td><td>23</td><td>14,5</td><td>0,6</td><td>0,5</td><td>GMIL</td><td>3</td></tr><tr><td>426</td><td>12,582</td><td>44,048</td><td>23,7</td><td>18,4</td><td>0,2</td><td>0,1</td><td>ITRN</td><td>3</td></tr><tr><td>427</td><td>9,84</td><td>44,073</td><td>22,7</td><td>15,5</td><td>0,1</td><td>0,1</td><td>LASP</td><td>3</td></tr><tr><td>428</td><td>15,228</td><td>44,113</td><td>22,4</td><td>17,9</td><td>0,4</td><td>0,5</td><td>ZADA</td><td>3</td></tr><tr><td>429</td><td>11,378</td><td>44,118</td><td>22</td><td>17,2</td><td>0,2</td><td>0,2</td><td>FIRE</td><td>3</td></tr><tr><td>430</td><td>11,113</td><td>44,122</td><td>22,9</td><td>16,7</td><td>0,1</td><td>0,1</td><td>BRAS</td><td>3</td></tr></table>
<table><caption>Table 3 – 468 velocity vectors from 1: this study, 2: Bonforte et al. [2014]; 3: Métois et al. [2015]; 4: Barreca et al. [2014]; 5: Musumeci et al. [2014]; 6: Ventura et al. [2014]; 7: Nocquet [2012]; 8: Devoti et al. [2011]; 9: Palano et al. [2015]; 10: Müller [2011]; 11: EUREF (www.euref.eu)</caption><tr><td>431</td><td>10,411</td><td>44,133</td><td>23,3</td><td>17,5</td><td>0,9</td><td>1</td><td>FOSC</td><td>3</td></tr><tr><td>432</td><td>21,079</td><td>44,153</td><td>23,6</td><td>14,2</td><td>0,3</td><td>0,4</td><td>BATO</td><td>3</td></tr><tr><td>433</td><td>9,769</td><td>44,194</td><td>22,5</td><td>15,2</td><td>0,2</td><td>0,4</td><td>BEVE</td><td>3</td></tr><tr><td>434</td><td>11,766</td><td>44,225</td><td>23,5</td><td>18,8</td><td>0,2</td><td>0,3</td><td>BRIS</td><td>3</td></tr><tr><td>435</td><td>9,725</td><td>44,236</td><td>22</td><td>15,6</td><td>0,4</td><td>0,9</td><td>BRUG</td><td>3</td></tr><tr><td>436</td><td>11,148</td><td>44,265</td><td>23,2</td><td>18,1</td><td>0,1</td><td>0,2</td><td>GRZM</td><td>3</td></tr><tr><td>437</td><td>19,884</td><td>44,272</td><td>22,8</td><td>15,5</td><td>0,3</td><td>0,3</td><td>VALJ</td><td>3</td></tr><tr><td>438</td><td>11,111</td><td>44,287</td><td>24,1</td><td>16,7</td><td>0,1</td><td>0,1</td><td>VERG</td><td>3</td></tr><tr><td>439</td><td>11,861</td><td>44,303</td><td>23</td><td>18,6</td><td>0,2</td><td>0,3</td><td>FAEZ</td><td>3</td></tr><tr><td>440</td><td>11,425</td><td>44,313</td><td>23,6</td><td>20,6</td><td>0,3</td><td>0,5</td><td>MTRZ</td><td>3</td></tr><tr><td>441</td><td>9,324</td><td>44,32</td><td>22,5</td><td>15,4</td><td>0,2</td><td>0,3</td><td>CHIV</td><td>3</td></tr><tr><td>442</td><td>11,718</td><td>44,347</td><td>23,8</td><td>18,5</td><td>0,2</td><td>0,3</td><td>ITIM</td><td>3</td></tr><tr><td>443</td><td>12,192</td><td>44,405</td><td>23,9</td><td>17,7</td><td>0,4</td><td>0,4</td><td>RAVE</td><td>3</td></tr><tr><td>444</td><td>10,278</td><td>44,411</td><td>23,2</td><td>16,2</td><td>0,3</td><td>0,6</td><td>RAMS</td><td>3</td></tr><tr><td>445</td><td>8,921</td><td>44,419</td><td>22,7</td><td>15,1</td><td>0,1</td><td>0,1</td><td>GENO</td><td>3</td></tr><tr><td>446</td><td>10,405</td><td>44,432</td><td>22,9</td><td>17,2</td><td>0,1</td><td>0,3</td><td>CAST</td><td>3</td></tr><tr><td>447</td><td>9,766</td><td>44,488</td><td>22,7</td><td>16,2</td><td>0,1</td><td>0,2</td><td>TARO</td><td>3</td></tr><tr><td>448</td><td>11,351</td><td>44,511</td><td>23,4</td><td>18,1</td><td>0,2</td><td>0,2</td><td>BLGN</td><td>3</td></tr><tr><td>449</td><td>11,646</td><td>44,52</td><td>23,7</td><td>17,6</td><td>0,1</td><td>0,1</td><td>MSEL</td><td>3</td></tr><tr><td>450</td><td>11,647</td><td>44,52</td><td>22,7</td><td>16,3</td><td>0,2</td><td>0,2</td><td>MEDI</td><td>9</td></tr><tr><td>451</td><td>19,225</td><td>44,535</td><td>24,3</td><td>16</td><td>0,3</td><td>0,4</td><td>LOZN</td><td>3</td></tr><tr><td>452</td><td>10,949</td><td>44,629</td><td>23,1</td><td>18,6</td><td>0,1</td><td>0,2</td><td>MODE</td><td>3</td></tr><tr><td>453</td><td>11,183</td><td>44,636</td><td>23,9</td><td>16,6</td><td>0,2</td><td>0,2</td><td>SGIP</td><td>3</td></tr><tr><td>454</td><td>20,753</td><td>44,642</td><td>22,4</td><td>15</td><td>0,4</td><td>0,4</td><td>GROC</td><td>3</td></tr><tr><td>455</td><td>11,19</td><td>44,645</td><td>23,5</td><td>18,1</td><td>0,2</td><td>0,3</td><td>PERS</td><td>3</td></tr><tr><td>456</td><td>12,249</td><td>44,677</td><td>22,9</td><td>16,4</td><td>0,2</td><td>0,2</td><td>GARI</td><td>3</td></tr><tr><td>457</td><td>10,637</td><td>44,706</td><td>24,2</td><td>17</td><td>0,1</td><td>0,1</td><td>REGG</td><td>3</td></tr><tr><td>458</td><td>10,216</td><td>44,753</td><td>22,7</td><td>17,3</td><td>0,2</td><td>0,2</td><td>COLL</td><td>3</td></tr><tr><td>459</td><td>10,312</td><td>44,765</td><td>23,4</td><td>16,7</td><td>0,1</td><td>0,2</td><td>PARM</td><td>3</td></tr><tr><td>460</td><td>21,52</td><td>44,767</td><td>22,9</td><td>14,4</td><td>0,2</td><td>0,3</td><td>VGRA</td><td>3</td></tr><tr><td>461</td><td>9,383</td><td>44,771</td><td>23,1</td><td>16</td><td>0,1</td><td>0,3</td><td>BOBB</td><td>3</td></tr><tr><td>462</td><td>20,477</td><td>44,806</td><td>22,9</td><td>14,8</td><td>0,2</td><td>0,2</td><td>BEOG</td><td>3</td></tr><tr><td>463</td><td>11,627</td><td>44,814</td><td>22,9</td><td>16,5</td><td>0,1</td><td>0,1</td><td>FERA</td><td>3</td></tr><tr><td>464</td><td>9,197</td><td>44,823</td><td>22,5</td><td>15,7</td><td>0,2</td><td>0,2</td><td>VARZ</td><td>3</td></tr><tr><td>465</td><td>11,601</td><td>44,828</td><td>23,2</td><td>16,8</td><td>0,2</td><td>0,2</td><td>FERI</td><td>3</td></tr><tr><td>466</td><td>12,112</td><td>44,837</td><td>22,7</td><td>17</td><td>0,2</td><td>0,1</td><td>CODI</td><td>3</td></tr><tr><td>467</td><td>10,662</td><td>44,918</td><td>22,4</td><td>16,4</td><td>0,1</td><td>0,1</td><td>GUAS</td><td>3</td></tr><tr><td>468</td><td>12,334</td><td>44,952</td><td>22,6</td><td>16,8</td><td>0,2</td><td>0,2</td><td>PTOI</td><td>3</td></tr></table>
B HISTORICAL EARTHQUAKES

<table><thead><tr><td>Reference</td><td>Yr</td><td>Month</td><td>Day</td><td>Latitude</td><td>Longitude</td><td>Depth</td><td>Magnitude</td></tr></thead><tbody><tr><td>1</td><td>17</td><td></td><td></td><td>37,8</td><td>15,2</td><td>0</td><td>5,1</td></tr><tr><td>2</td><td>361</td><td></td><td></td><td>37,5</td><td>14</td><td>0</td><td>6,6</td></tr><tr><td>3</td><td>701</td><td></td><td></td><td>37,583</td><td>12,833</td><td>0</td><td>5,8</td></tr><tr><td>4</td><td>1125</td><td>6</td><td>7</td><td>37,083</td><td>15,283</td><td>0</td><td>5,8</td></tr><tr><td>5</td><td>1169</td><td>2</td><td>4</td><td>37,217</td><td>14,95</td><td>0</td><td>6,4</td></tr><tr><td>2</td><td>1295</td><td></td><td></td><td>37,5</td><td>14</td><td>0</td><td>5,8</td></tr><tr><td>6</td><td>1536</td><td>3</td><td>23</td><td>37,502</td><td>15,087</td><td>10</td><td>5</td></tr><tr><td>6</td><td>1537</td><td>5</td><td></td><td>37,502</td><td>15,087</td><td>10</td><td>4,6</td></tr><tr><td>59</td><td>1542</td><td>12</td><td>10</td><td>37,233</td><td>15,017</td><td>0</td><td>6,8</td></tr><tr><td>7</td><td>1566</td><td>11</td><td>30</td><td>37,877</td><td>14,948</td><td>10</td><td>4,6</td></tr><tr><td>8</td><td>1578</td><td></td><td></td><td>37,508</td><td>13,083</td><td>10</td><td>5,2</td></tr><tr><td>9</td><td>1613</td><td>8</td><td>25</td><td>38,117</td><td>14,783</td><td>0</td><td>5,6</td></tr><tr><td>10</td><td>1624</td><td>10</td><td>3</td><td>37,27</td><td>14,75</td><td>10</td><td>5,6</td></tr><tr><td>63</td><td>1633</td><td>2</td><td>21</td><td>37,62</td><td>15,03</td><td>10</td><td>4,8</td></tr><tr><td>11</td><td>1643</td><td>7</td><td>17</td><td>37,783</td><td>14,599</td><td>10</td><td>5</td></tr><tr><td>63</td><td>1669</td><td>3</td><td>10</td><td>37,62</td><td>15,03</td><td>10</td><td>4,8</td></tr><tr><td>12</td><td>1693</td><td>1</td><td>9</td><td>37,133</td><td>15,033</td><td>0</td><td>6,2</td></tr><tr><td>12</td><td>1693</td><td>1</td><td>11</td><td>37,133</td><td>15,017</td><td>0</td><td>7,4</td></tr><tr><td>6</td><td>1716</td><td>12</td><td>1</td><td>37,502</td><td>15,087</td><td>10</td><td>5,2</td></tr><tr><td>13</td><td>1717</td><td></td><td></td><td>38,1</td><td>15,217</td><td>0</td><td>5</td></tr><tr><td>65</td><td>1718</td><td>2</td><td>20</td><td>37,599</td><td>14,619</td><td>150</td><td>5,4</td></tr><tr><td>15</td><td>1726</td><td></td><td></td><td>38,117</td><td>13,35</td><td>0</td><td>5,6</td></tr><tr><td>16</td><td>1727</td><td>5</td><td>8</td><td>37,5</td><td>13</td><td>10</td><td>4,8</td></tr><tr><td>17</td><td>1739</td><td>5</td><td>10</td><td>38,1</td><td>14,75</td><td>0</td><td>5,1</td></tr><tr><td>3</td><td>1740</td><td>6</td><td>13</td><td>37,582</td><td>12,84</td><td>10</td><td>5,4</td></tr><tr><td>18</td><td>1780</td><td>9</td><td>14</td><td>38,083</td><td>14,983</td><td>0</td><td>5,4</td></tr><tr><td>19</td><td>1786</td><td></td><td></td><td>38,1</td><td>15,017</td><td>0</td><td>6,2</td></tr><tr><td>8</td><td>1817</td><td>1</td><td>14</td><td>37,508</td><td>13,083</td><td>10</td><td>4,6</td></tr><tr><td>20</td><td>1818</td><td>2</td><td>20</td><td>37,6</td><td>15,13</td><td>150</td><td>6</td></tr><tr><td>21</td><td>1818</td><td>3</td><td>1</td><td>37,2</td><td>14,75</td><td>0</td><td>5,5</td></tr><tr><td>22</td><td>1819</td><td></td><td></td><td>37,933</td><td>14,05</td><td>0</td><td>5,3</td></tr><tr><td>10</td><td>1820</td><td>12</td><td>25</td><td>37,267</td><td>14,683</td><td>10</td><td>4,8</td></tr><tr><td>23</td><td>1822</td><td>4</td><td>6</td><td>37,747</td><td>14,398</td><td>10</td><td>5</td></tr><tr><td>24</td><td>1823</td><td>3</td><td>27</td><td>37,931</td><td>12,329</td><td>150</td><td>5,2</td></tr><tr><td>25</td><td>1828</td><td>5</td><td>18</td><td>37,8</td><td>12,433</td><td>150</td><td>5,2</td></tr><tr><td>16</td><td>1831</td><td>12</td><td>16</td><td>37,5</td><td>13,083</td><td>10</td><td>4,8</td></tr><tr><td>6,3</td><td>1846</td><td>4</td><td>22</td><td>37,502</td><td>15,087</td><td>10</td><td>4,6</td></tr><tr><td>20</td><td>1848</td><td></td><td></td><td>37,55</td><td>15,1</td><td>0</td><td>5,5</td></tr><tr><td>62</td><td>1850</td><td>1</td><td>1</td><td>37,617</td><td>14,923</td><td>10</td><td>4,6</td></tr><tr><td>64</td><td>1855</td><td>1</td><td>26</td><td>37,724</td><td>15,147</td><td>10</td><td>4,6</td></tr><tr><td>64</td><td>1865</td><td>7</td><td>19</td><td>37,702</td><td>15,153</td><td>10</td><td>5</td></tr><tr><td>26</td><td>1876</td><td>5</td><td>25</td><td>37,817</td><td>13,3</td><td>150</td><td>4,8</td></tr><tr><td>27</td><td>1878</td><td>10</td><td>4</td><td>37,266</td><td>14,691</td><td>10</td><td>5</td></tr><tr><td>60</td><td>1879</td><td>6</td><td>17</td><td>37,669</td><td>15,136</td><td>10</td><td>4,8</td></tr><tr><td>61</td><td>1889</td><td>12</td><td>25</td><td>37,651</td><td>15,156</td><td>10</td><td>4,6</td></tr><tr><td>28</td><td>1894</td><td>2</td><td>20</td><td>37,925</td><td>15,076</td><td>10</td><td>4,6</td></tr></tbody></table>
<table><caption>Table 4 – Historical earthquakes from Lavecchia et al. [2007] and from the CFTI catalog (http://storing.ingv.it/cfti4med/)</caption><tr><td>61</td><td>1894</td><td>8</td><td>8</td><td>37,653</td><td>15,11</td><td>10</td><td>4,8</td></tr><tr><td>58</td><td>1898</td><td>5</td><td>14</td><td>37,615</td><td>14,889</td><td>10</td><td>4,6</td></tr><tr><td>62</td><td>1898</td><td>11</td><td>2</td><td>37,216</td><td>14,495</td><td>10</td><td>4,6</td></tr><tr><td>29</td><td>1903</td><td>7</td><td>13</td><td>37,15</td><td>14,4</td><td>10</td><td>4,6</td></tr><tr><td>30</td><td>1907</td><td>4</td><td>24</td><td>37,633</td><td>13,637</td><td>150</td><td>4,6</td></tr><tr><td>31</td><td>1907</td><td>5</td><td>8</td><td>37,5</td><td>15</td><td>10</td><td>5,2</td></tr><tr><td>61</td><td>1907</td><td>12</td><td>7</td><td>37,632</td><td>15,134</td><td>10</td><td>4,6</td></tr><tr><td>32</td><td>1908</td><td></td><td></td><td>38,15</td><td>15,683</td><td>0</td><td>7,1</td></tr><tr><td>26</td><td>1909</td><td>1</td><td>2</td><td>37,233</td><td>14,5</td><td>10</td><td>4,8</td></tr><tr><td>33</td><td>1909</td><td>6</td><td>7</td><td>37,817</td><td>13,3</td><td>150</td><td>4,8</td></tr><tr><td>34</td><td>1909</td><td>12</td><td>3</td><td>37,9</td><td>13,1</td><td>150</td><td>4,6</td></tr><tr><td>10</td><td>1911</td><td>10</td><td>15</td><td>37,699</td><td>15,154</td><td>10</td><td>4,8</td></tr><tr><td>64</td><td>1911</td><td>10</td><td>29</td><td>37,267</td><td>14,683</td><td>10</td><td>4,6</td></tr><tr><td>61</td><td>1914</td><td>5</td><td>8</td><td>37,659</td><td>15,149</td><td>10</td><td>5,3</td></tr><tr><td>64</td><td>1920</td><td>9</td><td>26</td><td>37,713</td><td>15,161</td><td>10</td><td>4,6</td></tr><tr><td>6</td><td>1921</td><td>7</td><td>24</td><td>37,517</td><td>15,083</td><td>10</td><td>4,8</td></tr><tr><td>35</td><td>1925</td><td>8</td><td>21</td><td>37,683</td><td>14,567</td><td>150</td><td>4,8</td></tr><tr><td>36</td><td>1927</td><td>9</td><td>22</td><td>37,7</td><td>13,9</td><td>150</td><td>4,8</td></tr><tr><td>37</td><td>1933</td><td>2</td><td>26</td><td>37,559</td><td>13,17</td><td>10</td><td>4,6</td></tr><tr><td>38</td><td>1934</td><td>9</td><td>11</td><td>37,439</td><td>14,58</td><td>150</td><td>5</td></tr><tr><td>39</td><td>1940</td><td></td><td></td><td>38,083</td><td>13,433</td><td>0</td><td>5,3</td></tr><tr><td>61</td><td>1950</td><td>4</td><td>8</td><td>37,707</td><td>15,164</td><td>10</td><td>4,6</td></tr><tr><td>61</td><td>1952</td><td>3</td><td>19</td><td>37,66</td><td>15,147</td><td>10</td><td>4,6</td></tr><tr><td>40</td><td>1954</td><td>11</td><td>20</td><td>37,925</td><td>13,094</td><td>150</td><td>4,8</td></tr><tr><td>41</td><td>1959</td><td>12</td><td>23</td><td>37,428</td><td>14,89</td><td>150</td><td>5,2</td></tr><tr><td>42</td><td>1967</td><td>9</td><td>7</td><td>37,9</td><td>15,3</td><td>10</td><td>4,8</td></tr><tr><td>43</td><td>1968</td><td>1</td><td>14</td><td>37,804</td><td>13,012</td><td>19</td><td>5,2</td></tr><tr><td>43</td><td>1968</td><td>1</td><td>15</td><td>37,75</td><td>12,983</td><td>13</td><td>6,1</td></tr><tr><td>44</td><td>1968</td><td>1</td><td>16</td><td>37,857</td><td>12,976</td><td>36</td><td>5,2</td></tr><tr><td>45</td><td>1968</td><td>1</td><td>25</td><td>37,687</td><td>12,966</td><td>3</td><td>5,2</td></tr><tr><td>46</td><td>1968</td><td>9</td><td>1</td><td>37,8</td><td>13</td><td>150</td><td>4,6</td></tr><tr><td>47</td><td>1970</td><td>12</td><td>30</td><td>37,7</td><td>12,9</td><td>150</td><td>4,6</td></tr><tr><td>64</td><td>1971</td><td>4</td><td>21</td><td>37,714</td><td>15,148</td><td>10</td><td>4,8</td></tr><tr><td>48</td><td>1972</td><td>12</td><td>27</td><td>37,701</td><td>13,021</td><td>10</td><td>4,8</td></tr><tr><td>48</td><td>1973</td><td>9</td><td>21</td><td>37,7</td><td>13</td><td>150</td><td>4,8</td></tr><tr><td>49</td><td>1975</td><td>6</td><td>12</td><td>37,45</td><td>14,433</td><td>150</td><td>4,6</td></tr><tr><td>50</td><td>1976</td><td>10</td><td>12</td><td>37,833</td><td>13,067</td><td>150</td><td>4,6</td></tr><tr><td>51</td><td>1978</td><td>1</td><td>19</td><td>37,583</td><td>14,1</td><td>150</td><td>4,6</td></tr><tr><td>52</td><td>1978</td><td></td><td></td><td>38,117</td><td>15,017</td><td>0</td><td>5,7</td></tr><tr><td>53</td><td>1981</td><td>6</td><td>7</td><td>37,67</td><td>12,47</td><td>18,1</td><td>4,6</td></tr><tr><td>20</td><td>1984</td><td>10</td><td>25</td><td>37,575</td><td>15,124</td><td>5,9</td><td>4,7</td></tr><tr><td>54</td><td>1987</td><td>2</td><td>2</td><td>37,766</td><td>14,702</td><td>26,9</td><td>4,7</td></tr><tr><td>55</td><td>1987</td><td>8</td><td>13</td><td>37,9</td><td>15,06</td><td>35,9</td><td>4</td></tr><tr><td>56</td><td>1988</td><td>10</td><td>28</td><td>37,812</td><td>15,068</td><td>0,2</td><td>4,5</td></tr><tr><td>57</td><td>1990</td><td>12</td><td>13</td><td>37,267</td><td>14,983</td><td>0</td><td>5,4</td></tr><tr><td>14</td><td>1999</td><td>8</td><td>30</td><td>37,532</td><td>14,638</td><td>28,6</td><td>4,9</td></tr><tr><td>60</td><td>2002</td><td>10</td><td>29</td><td>37,68</td><td>15,1</td><td>1,32</td><td>4,5</td></tr></table>
C TIME SERIES OF RING STATION

<figure><img src="image_27.png" /></figure>

<figure><img src="image_28.png" /></figure>

<figure><img src="image_29.png" /></figure>

<figure><img src="image_30.png" /></figure>

<figure><img src="image_31.png" /></figure>

<figure><img src="image_32.png" /></figure>

<figure><img src="image_33.png" /></figure>

<figure><img src="image_34.png" /></figure>

<figure><img src="image_35.png" /></figure>

<figure><img src="image_36.png" /></figure>

<figure><img src="image_37.png" /></figure>

<figure><img src="image_38.png" /></figure>

<figure><img src="image_39.png" /></figure>

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<figure><img src="image_45.png" /></figure>

<figure><img src="image_46.png" /></figure>

<figure><img src="image_47.png" /></figure>
<figure><img src="image_48.png" /><figcaption>Figure 25 – Time series of RING stations. a/ East component; b/ North component; c/ Up component</figcaption></figure>