cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.6084/m9.figshare.16918066
title: Petrology and geochemistry of ultramafic and mafic rocks in the late Silurian-early Devonian Darbut ophiolitic mélange of west Junggar (NORTHWESTERN CHINA): implications for petrogenesis and tectonic evolution

description: New petrological and geochemical data for lherzolite, harzburgite, and gabbros in the Darbut ophiolitic mélange of west Junggar are combined to constrain the geological evolution of the Darbut ophiolite. Lherzolite, consisting of olivine, orthopyroxene, clinopyroxene, and chrome–spinel with low Cr# values (34–39), is analogous to fertile abyssal peridotite. Harzburgite, composed of olivine, orthopyroxene, clinopyroxene, and chrome–spinel with relatively high Cr# values (48–55), is similar to the supra–subduction zone (SSZ) peridotite. Isotropic gabbro, characterized by a flat rare earth element (REE) pattern as well as low Nb/Yb and high Ti/V ratios, is comparable to mid–ocean ridge basalt (MORB). Hornblende gabbro, displaying relative enrichments of fluid-soluble elements and elevated Th/Yb ratios, is similar to that of fore–arc basalt. Geochemical modelling of partial melting suggests that lherzolite samples are compatible with their formation after relatively low-degree (11–16%), anhydrous dynamic melting of the primitive mantle, while harzburgite samples have undergone 5–10% secondary-stage partial melting based on the already 16% depleted primitive mantle. These data suggest that the Darbut ophiolite was generated in a forearc setting. The upwelling asthenosphere triggered by the subduction initiation of the Junggar oceanic lithosphere led to low-degree, anhydrous decompression melting, producing lherzolite as well as the MORB–like melts at Late Silurian period. Increasing slab–derived fluids influx, accompanied by the progressively sinking slab, largely enhanced the partial melting degrees of the depleted mantle, and formed refractory harzburgite.
DOI: 10.6084/m9.figshare.16918066.v2
title: Petrology and geochemistry of ultramafic and mafic rocks in the late Silurian-early Devonian Darbut ophiolitic mélange of west Junggar (NORTHWESTERN CHINA): implications for petrogenesis and tectonic evolution

description: New petrological and geochemical data for lherzolite, harzburgite, and gabbros in the Darbut ophiolitic mélange of west Junggar are combined to constrain the geological evolution of the Darbut ophiolite. Lherzolite, consisting of olivine, orthopyroxene, clinopyroxene, and chrome–spinel with low Cr# values (34–39), is analogous to fertile abyssal peridotite. Harzburgite, composed of olivine, orthopyroxene, clinopyroxene, and chrome–spinel with relatively high Cr# values (48–55), is similar to the supra–subduction zone (SSZ) peridotite. Isotropic gabbro, characterized by a flat rare earth element (REE) pattern as well as low Nb/Yb and high Ti/V ratios, is comparable to mid–ocean ridge basalt (MORB). Hornblende gabbro, displaying relative enrichments of fluid-soluble elements and elevated Th/Yb ratios, is similar to that of fore–arc basalt. Geochemical modelling of partial melting suggests that lherzolite samples are compatible with their formation after relatively low-degree (11–16%), anhydrous dynamic melting of the primitive mantle, while harzburgite samples have undergone 5–10% secondary-stage partial melting based on the already 16% depleted primitive mantle. These data suggest that the Darbut ophiolite was generated in a forearc setting. The upwelling asthenosphere triggered by the subduction initiation of the Junggar oceanic lithosphere led to low-degree, anhydrous decompression melting, producing lherzolite as well as the MORB–like melts at Late Silurian period. Increasing slab–derived fluids influx, accompanied by the progressively sinking slab, largely enhanced the partial melting degrees of the depleted mantle, and formed refractory harzburgite.
DOI: 10.6084/m9.figshare.17111429
title: Tectonic and petrogenetic settings of the Eocene Challis-Kamloops volcanic belt of western Canada and the northwestern United States

description: The Eocene Challis-Kamloops volcanic belt, which runs through the interior of British Columbia and northwest United States for &gt;2, 000 km, developed within a short time interval from ~55 to ~45 Ma. Volcanic rocks of the belt are discontinuously distributed in a series of grabens, half-grabens and calderas. Although predominantly composed of high- to medium-K calc-alkaline rocks that are typical of continental arcs, they were extruded during a time of regional transtensional tectonics in the Cordilleran orogen, which also led to the contemporaneous emplacement of Precambrian metamorphic core complexes near the belt. Their relative contents in Y, Nb, La, Sm, Gd, Yb and Ta suggest that the magmas were formed in relation to slab-failure (slab break-off). Initial Sr and Nd isotopic ratios and neodymium depleted mantle model ages indicate that the northern and southern parts of the belt had isotopically distinct lithospheric mantle sources with, respectively, Palaeozoic to Mesozoic and Precambrian model ages. As all rocks of the belt share common tectonic and petrogenetic settings, greater contents in incompatible trace elements in rocks from the southern part of the belt suggest that the Precambrian sources were more metasomatically enriched in these elements than the Phanerozoic sources.
DOI: 10.6084/m9.figshare.16799744.v1
title: First evidence for the subduction initiation and boninitic magmatism from the Armutlu Peninsula (NW Turkey): geodynamic significance for the Cadomian magmatic arc system of the Gondwanan margin

description: The Cadomian Orogeny was active along the northern margin of Gondwanaland during the Late Neoproterozoic–Early Cambrian period. Remains of this orogenic activity are traced from Western Europe to the Himalayas, including some metamorphic basement rocks of Turkey. In this study, we provide new whole-rock and mineral chemistry, and zircon U–Pb age data for the metagabbro and metagranites in the Armutlu Peninsula, north of the Intra Pontide suture zone (IPSZ), which are the equivalent of the Cadomian basement of the İstanbul Zone (İZ). Geochemically, the metagabbros show an extreme depletion in Nb, Zr, Th, and Hf; low TiO<sub>2</sub> contents; and high Mg# values exhibiting boninitic affinity, which are commonly associated with fore-arc settings. The metagranites are calc-alkaline and high-K calc-alkaline in character. They are slightly enriched in LREE and have similar features to shear-type plagiogranites. The yielded zircon U-Pb crystallization ages are 564 ± 4.4 Ma for metagabbros and 561 ± 9.5 Ma (Late Ediacaran) for metagranites. In this study, we provide additional information for the Cadomian basement of the İZ and the geodynamic evolution of Cadomian magmatism by discussing the tectonic setting for two geochemically contrast but almost coeval magmatic products.
DOI: 10.6084/m9.figshare.16918066.v1
title: Petrology and geochemistry of ultramafic and mafic rocks in the late Silurian-early Devonian darbut ophiolitic mélange of west Junggar (NORTHWESTERN CHINA): implications for petrogenesis and tectonic evolution

description: New petrological and geochemical data for lherzolite, harzburgite, and gabbros in the Darbut ophiolitic mélange of west Junggar are combined to constrain the geological evolution of the Darbut ophiolite. Lherzolite, consisting of olivine, orthopyroxene, clinopyroxene, and chrome–spinel with low Cr# values (34–39), is analogous to fertile abyssal peridotite. Harzburgite, composed of olivine, orthopyroxene, clinopyroxene, and chrome–spinel with relatively high Cr# values (48–55), is similar to the supra–subduction zone (SSZ) peridotite. Isotropic gabbro, characterized by a flat rare earth element (REE) pattern as well as low Nb/Yb and high Ti/V ratios, is comparable to mid–ocean ridge basalt (MORB). Hornblende gabbro, displaying relative enrichments of fluid-soluble elements and elevated Th/Yb ratios, is similar to that of fore–arc basalt. Geochemical modelling of partial melting suggests that lherzolite samples are compatible with their formation after relatively low-degree (11–16%), anhydrous dynamic melting of the primitive mantle, while harzburgite samples have undergone 5–10% secondary-stage partial melting based on the already 16% depleted primitive mantle. These data suggest that the Darbut ophiolite was generated in a forearc setting. The upwelling asthenosphere triggered by the subduction initiation of the Junggar oceanic lithosphere led to low-degree, anhydrous decompression melting, producing lherzolite as well as the MORB–like melts at Late Silurian period. Increasing slab–derived fluids influx, accompanied by the progressively sinking slab, largely enhanced the partial melting degrees of the depleted mantle, and formed refractory harzburgite.
DOI: 10.6084/m9.figshare.17026705
title: Quantifying crustal thickness and magmatic temperatures of the Jurassic to Early Cretaceous North-Andean arc

description: We characterized the crustal thickness variations and magmatic saturation temperatures of the Early Jurassic to Early Cretaceous (194–130 Ma) plutonic and volcanic rocks of the Northern Andes of Colombia and Ecuador, combining trace elements signatures and zircon and apatite saturation temperatures. Also, we analysed the implications of the emplacement conditions during the last stage of the magmatism using Al-in-hornblende thermobarometry. Moderate rare earth elements (REE) slopes and depleted heavy REE patterns show that the primary residual magma source was amphibole, but plagioclase and pyroxene were also significant residual phases indicating that the magma source was formed in a crust that varied in thickness from 35 to 50 km. According to the La/Yb and Sr/Y crustal quantifications and the REE ratios, two phases in the arc evolution are characterized by a thick crust. The first is in Santa Marta Massif, Upper Magdalena Valley and Garzón Massif (190–180 Ma), which could be associated with shortening or basaltic underplating due to magmatic events. The second one recorded in the Ibagué Batholith (160–154 Ma) is related to the crustal thickening on an oblique subduction setting. During the latter period, the magmatic volumes progressively decreased, as is recorded by saturation temperatures increase. Finally, a thin crust emplaced the last stage of the arc magmatism during the Late Jurassic to Early Cretaceous (154–130 Ma).
DOI: 10.6084/m9.figshare.17026705.v1
title: Quantifying crustal thickness and magmatic temperatures of the Jurassic to Early Cretaceous North-Andean arc

description: We characterized the crustal thickness variations and magmatic saturation temperatures of the Early Jurassic to Early Cretaceous (194–130 Ma) plutonic and volcanic rocks of the Northern Andes of Colombia and Ecuador, combining trace elements signatures and zircon and apatite saturation temperatures. Also, we analysed the implications of the emplacement conditions during the last stage of the magmatism using Al-in-hornblende thermobarometry. Moderate rare earth elements (REE) slopes and depleted heavy REE patterns show that the primary residual magma source was amphibole, but plagioclase and pyroxene were also significant residual phases indicating that the magma source was formed in a crust that varied in thickness from 35 to 50 km. According to the La/Yb and Sr/Y crustal quantifications and the REE ratios, two phases in the arc evolution are characterized by a thick crust. The first is in Santa Marta Massif, Upper Magdalena Valley and Garzón Massif (190–180 Ma), which could be associated with shortening or basaltic underplating due to magmatic events. The second one recorded in the Ibagué Batholith (160–154 Ma) is related to the crustal thickening on an oblique subduction setting. During the latter period, the magmatic volumes progressively decreased, as is recorded by saturation temperatures increase. Finally, a thin crust emplaced the last stage of the arc magmatism during the Late Jurassic to Early Cretaceous (154–130 Ma).
DOI: 10.6084/m9.figshare.17111429.v1
title: Tectonic and petrogenetic settings of the Eocene Challis-Kamloops volcanic belt of western Canada and the northwestern United States

description: The Eocene Challis-Kamloops volcanic belt, which runs through the interior of British Columbia and northwest United States for &gt;2, 000 km, developed within a short time interval from ~55 to ~45 Ma. Volcanic rocks of the belt are discontinuously distributed in a series of grabens, half-grabens and calderas. Although predominantly composed of high- to medium-K calc-alkaline rocks that are typical of continental arcs, they were extruded during a time of regional transtensional tectonics in the Cordilleran orogen, which also led to the contemporaneous emplacement of Precambrian metamorphic core complexes near the belt. Their relative contents in Y, Nb, La, Sm, Gd, Yb and Ta suggest that the magmas were formed in relation to slab-failure (slab break-off). Initial Sr and Nd isotopic ratios and neodymium depleted mantle model ages indicate that the northern and southern parts of the belt had isotopically distinct lithospheric mantle sources with, respectively, Palaeozoic to Mesozoic and Precambrian model ages. As all rocks of the belt share common tectonic and petrogenetic settings, greater contents in incompatible trace elements in rocks from the southern part of the belt suggest that the Precambrian sources were more metasomatically enriched in these elements than the Phanerozoic sources.
DOI: 10.6084/m9.figshare.19573490.v1
title: Diachronous initiation of Arabia–Eurasia collision from eastern Anatolia to the southeastern Zagros Mountains since middle Eocene time

description: The persistent debate over the timing of initial Arabia–Eurasia collision has eluded consensus for decades, with most estimates ranging widely from ~50 to 10 Ma along both the Anatolian and Zagros segments of the orogen. Here, we independently evaluate the timing and location of initial collision using a quantitative plate tectonic reconstruction that is the first to include the entire Arabian microcontinent and regions to the north in eastern Anatolia, northwestern Iran, and the Caucasus. The reconstruction combines new kinematic constraints from recent global plate models with a synthesis of available constraints on crustal shortening and continental and back-arc subduction to restore the pre-collisional geometries of the Arabian and Eurasian continental margins and to track their interaction through time. Our preferred model suggests that initial continental underthrusting, or soft collision, of the relatively thin Arabian passive margin with Eurasia occurred by ca. 42 Ma along the eastern Bitlis suture zone and began transmitting strain across central and eastern Anatolia, the Caucasus, and northwestern Iran. Collision inception then propagated westward into central Anatolia and southeastward into the northwestern Zagros Mountains by late Eocene time (ca. 40–35 Ma), the central Zagros by latest Eocene to early Oligocene time, (ca. 35–25 Ma), and finally the southeastern Zagros by latest Oligocene to middle Miocene time (ca. 25–15 Ma). The diachroneity of Arabia collision led to widespread upper-plate (Eurasian) contraction and a similarly time-transgressive magmatic lull that lagged behind the onset of collision by ~2–12 Myr. By incorporating the entire Arabian microcontinent and regions to the north, this new tectonic reconstruction highlights the diachronous nature of Arabia–Eurasia collision that occurred first along the Bitlis suture zone in eastern Anatolia during late middle Eocene time and became progressively younger to the southeast along strike of the Zagros suture zone.
DOI: 10.14469/hpc/12343
title: Data for Papageorgiou&Tanveer 2023 ProcRoySoc

description: Data used to generate all figures appearing in the paper "Singular effect of interfacial slip for an otherwise stable two-layer shear flow: Analysis and computations" by Papageorgiou & Tanveer, Proc. R. Soc. 2023
DOI: 10.14469/hpc/12411
title: 1H NMR Spectrum For Eugenol Myristate

description: 1H NMR Spectrum For Eugenol Myristate - Synthesised During 1st Year Undergraduate Synthesis 1.2 Laboratory (2022-2023)
DOI: 10.34740/kaggle/dsv/5245440
title: AutoXGB
DOI: 10.5281/zenodo.7620795
title: Toloker Graph: Interaction of Crowd Annotators

description: The graph contains 11,758 nodes and 519,000 edges representing interactions between crowd annotators on a project labeled on the Toloka crowdsourcing platform (see the Toloka overview for the details on the used terminology). Each node represents an individual annotator; nodes are provided with four numerical and three categorical features. An edge is drawn between a pair of annotators if they annotated the same task. Also, each node is provided with a label showing whether the annotator was banned on this project, or not. <strong>Nodes</strong> are stored in the nodes.tsv file in the TSV format of the following structure: <code>id</code>: unique identifier of the annotator <code>approved_rate</code>: percentage of the approved labels of this annotator <code>skipped_rate</code>: percentage of the skipped tasks of this annotator <code>expired_rate</code>: percentage of the expired tasks of this annotator <code>rejected_rate</code>: percentage of the rejected labels of this annotator <code>education</code>: level of education as self-reported by this annotator (<code>none</code>, <code>basic</code>, <code>middle</code>, <code>high</code>) <code>english_profile</code>: knowledge of English as self-reported by this annotator (<code>0</code> for no, <code>1</code> for yes) <code>english_tested</code>: whether the annotator passed the Toloka language test for English (<code>0</code> for no, <code>1</code> for yes) <code>banned</code>: whether the annotator was banned on this project (<code>0</code> for no, <code>1</code> for yes) The <code>*_rate</code> attributes should sum up to 1. <strong>Edges</strong> are stored in the edges.tsv file in the TSV format of the following structure: <code>source</code>: source identifier of the annotator <code>target</code>: target identifier of the annotator As the graph is undirected, <code>source</code> and <code>target</code> can be interchanged for the given pair of nodes.
DOI: 10.5281/zenodo.7620796
title: Toloker Graph: Interaction of Crowd Annotators

description: The graph contains 11,758 nodes and 519,000 edges representing interactions between crowd annotators on a project labeled on the Toloka crowdsourcing platform (see the Toloka overview for the details on the used terminology). Each node represents an individual annotator; nodes are provided with four numerical and three categorical features. An edge is drawn between a pair of annotators if they annotated the same task. Also, each node is provided with a label showing whether the annotator was banned on this project, or not. <strong>Nodes</strong> are stored in the nodes.tsv file in the TSV format of the following structure: <code>id</code>: unique identifier of the annotator <code>approved_rate</code>: percentage of the approved labels of this annotator <code>skipped_rate</code>: percentage of the skipped tasks of this annotator <code>expired_rate</code>: percentage of the expired tasks of this annotator <code>rejected_rate</code>: percentage of the rejected labels of this annotator <code>education</code>: level of education as self-reported by this annotator (<code>none</code>, <code>basic</code>, <code>middle</code>, <code>high</code>) <code>english_profile</code>: knowledge of English as self-reported by this annotator (<code>0</code> for no, <code>1</code> for yes) <code>english_tested</code>: whether the annotator passed the Toloka language test for English (<code>0</code> for no, <code>1</code> for yes) <code>banned</code>: whether the annotator was banned on this project (<code>0</code> for no, <code>1</code> for yes) The <code>*_rate</code> attributes should sum up to 1. <strong>Edges</strong> are stored in the edges.tsv file in the TSV format of the following structure: <code>source</code>: source identifier of the annotator <code>target</code>: target identifier of the annotator As the graph is undirected, <code>source</code> and <code>target</code> can be interchanged for the given pair of nodes.
DOI: 10.34740/kaggle/dsv/5245331
title: RecipeNLG dataset
DOI: 10.5281/zenodo.7773589
title: CTD, LISST100X and Signature1000 data - 14/09/2021

description: CTD, LISST100X and Signature1000 profiles data collected at five stations (S1 to S5) along the Rhône River interflow in Lake Geneva on 14/09/2021.
DOI: 10.5281/zenodo.7773588
title: CTD, LISST100X and Signature1000 data - 14/09/2021

description: CTD, LISST100X and Signature1000 profiles data collected at five stations (S1 to S5) along the Rhône River interflow in Lake Geneva on 14/09/2021.
DOI: 10.6084/m9.figshare.22339693
title: Ueda 2023

description: Trapping location, mean distance from the SF line of each site, trapping periods, numbers of Nicrophorus nepalensis collected, location category and periods of observation on dead body of mouse and its consumers, number of mongooses caught per day per cylinder trap set within a 500 m radius in 2016-18, and canopy cover rates and forest condition at each trapping location
DOI: 10.6084/m9.figshare.22339693.v1
title: Ueda 2023

description: Trapping location, mean distance from the SF line of each site, trapping periods, numbers of Nicrophorus nepalensis collected, location category and periods of observation on dead body of mouse and its consumers, number of mongooses caught per day per cylinder trap set within a 500 m radius in 2016-18, and canopy cover rates and forest condition at each trapping location
DOI: 10.5281/zenodo.7696671
title: LawSampo Knowledge Graph

description: The LawSampo Knowledge Graph contains Finnish consolidated legislation and case law as Linked Open Data. This dataset is available on a public SPARQL endpoint (<em>http://ldf.fi/lawsampo/sparql</em>). To test and demonstrate its usefulness, this Knowledge Graph is in use in the semantic portal LawSampo, explained in more detail in the project page. See the dataset page on LDF.fi for more details.
DOI: 10.5281/zenodo.7696672
title: LawSampo Knowledge Graph

description: The LawSampo Knowledge Graph contains Finnish consolidated legislation and case law as Linked Open Data. This dataset is available on a public SPARQL endpoint (<em>http://ldf.fi/lawsampo/sparql</em>). To test and demonstrate its usefulness, this Knowledge Graph is in use in the semantic portal LawSampo, explained in more detail in the project page. See the dataset page on LDF.fi for more details.
DOI: 10.6084/m9.figshare.22339594.v1
title: Figure 3

description: It comprises of raw data and analysis file of Figure 3 obtained by assessing the molecular components in the MRMT1 CM responsible for PC12 neuritogenesis. PC12 cells were treated with unfractionated MRMT1 CM (whole fraction, WF), &gt;3kDa fraction and &lt;3kDa fractio for 72 h and neurite growth from PC12 cells was quantified. Data obtained from CM fractions were normalized to parameters from the whole fraction group, performed in triplicates.