cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.15151/esrf-es-772926630
title: Offretite and laumontite at non-ambient conditions

description: While the high-pressure and high-temperature behavior of natural zeolites has been intensively studied in the last decades by several researchers, to the best of our knowledge, no in-situ X-ray diffraction studies have been performed combining the effects of both. Experiments at these conditions could have crucial geological implications: during the early stages of the diagenetic process (i.e., zeolite facies), both pressure (P) and temperature (T) increase, following different thermal gradient (e.g., about 25°C/Km for the first few kilometers of the continental crust). In this proposal, the PT behavior of two natural zeolites, laumontite ([(Ca4-xNax)Kx][Al8Si16O48]⋅(H2O)n, with n &lt; 16) and offretite (K, Ca, Mg) Si13Al5O36 ·15H2O which occur in a wide range of natural environments, including sedimentary deposits or volcanoclastic sequences interested by burial diagenesis/metamorphism, as well as in hydrothermal vugs of volcanic rocks.
DOI: 10.15151/esrf-es-735689281
title: Local atomic order and Mbar pressure-temperature phase diagram of BaZrO3 perovskite

description: Information on the local scale and structural stability of cubic ABO3 perovskite still lacks systematic detailing. BaZrO3 is a widely explored material for several applications due to its interesting properties. However, its structural stability under pressure still raises great doubts. This topic is considered a challenge, especially when related to the possible phase transition also at low temperature. The lack of detailed structural data along with the small amount of previous studies on the phase transitions of BaZrO3 makes this topic an interesting to be explored. Therefore, we propose here to study the phase transition under pressure Pm-3m to I4/mcm in BaZrO3 perovskite and to probe its pressure-temperature phase diagram, considering runs at low temperature (10‒300K) and high-pressure (0‒1Mbar). This will provide information on crystal structure stability of BaZrO3 perovskite.
DOI: 10.48370/ofd/dyxzps/fcu19t
title: Teratoclytus plavilstshikovi (2).JPG

description: :unav
DOI: 10.48370/ofd/dyxzps
title: Teratoclytus plavilstshikovi (Zeitzev, 1937), C-856

description: Coleoptera collection
DOI: 10.48370/ofd/n2jwm3/tbxu8k
title: Cleroclytus semirufus (2).JPG

description: :unav
DOI: 10.48370/ofd/n2jwm3
title: Cleroclytus semirufus (Kraatz, 1884), C-857

description: Coleoptera collection
DOI: 10.48370/ofd/dsnxgc
title: Cleroclytus semirufus (Kraatz, 1884), C-858

description: Coleoptera collection
DOI: 10.6084/m9.figshare.17128452.v1
title: Role of Late Cretaceous volcanic-sedimentary melanges, specifically the Aladağ melange, E Turkey, in the rift-drift-subduction-accretion-emplacement history of the Tethyan Inner Tauride ocean

description: The Aladağ melange is located between Mesozoic Tauride carbonate platform units and the Late Cretaceous Pozantı-Karsantı ophiolite and its metamorphic sole. The melange comprises a lower, mainly sedimentary unit, composed of variably disrupted thrust sheets of deep-sea sediments, with a localized matrix of mass-flow and turbidity current deposits. The upper, volcanic-sedimentary melange comprises highly disrupted basalt-pelagic carbonate-radiolarite units, rarely associated with gravity-flow deposits. Tholeiitic to alkaline basalts in the melange range from N-MORB, to E-MORB and to OIB, and are dated as Middle Jurassic to Early Cretaceous using Radiolaria from interbedded pelagic sediments. Comparisons with accretionary melanges throughout southern Turkey and elsewhere indicate a similar geochemical pattern of variable ‘enrichment’, commonly coupled with a subduction influence (e.g. negative Nb, Ta anomalies). Geochemically, the subduction-influenced basalts are consistent with an oceanic island arc origin. However, the geological setting of Triassic basalts within some of the melanges (e.g. Mersin) is indicative of a rifted continental margin setting. The Mesozoic basalts within the Turkish melanges considered here erupted along the distal, outer northern margin of the Tauride continent, followed by Late Cretaceous subduction-accretion and supra-subduction zone ophiolite emplacement. Regional to global chemical comparisons suggest that the subduction influence could represent geochemical subduction inheritance rather than contemporaneous subduction.
DOI: 10.6084/m9.figshare.14535512
title: Neoproterozoic geodynamics in NW India – evidence from Erinpura granites in the South Delhi Fold Belt

description: Erinpura Granites form the basement for the Neoproterozoic Malani Igneous Suite in NW India. Based on this study, the Erinpura granites can be divided into Erinpura-East (gneissic fabric), a belt parallel to the southern sector of the South Delhi Fold Belt, and Erinpura-West (magmatic fabrics). EPMA dating on monazites gives a time frame of 890 to 860 Ma for crystallization of both types. The geochemically homogeneous peraluminous S-type granites with ε<sub>Nd</sub> values of −2.1 to −10.8 are interpreted as melting products of Archaean crust. REE pattern follows the pattern of the average continental crust, but Erinpura-East samples are more fractionated with steeper HREE depletion indicating melting in a deeper crustal level. A thermal pulse between 835 and 820 Ma constrains the timing of deformation in granite-gneisses during uplift along thrust planes, coeval with shear-bound exhumation of high-grade metamorphic rocks and initiated by delamination of the lower crust in this southern sector of the South Delhi Fold Belt. This is in contrast to the northern sector of the SDFB with arrested orogenic development and without considerable delamination or erosion of the lower crust. Latest movement related to the 200 Ma tectono-magmatic history overlaps with initiation of rifting during the Malani igneous event. A change from S-type to A-type granites and shift of isotopic signatures to ε<sub>Nd</sub> values of −2.8 to −1.7 indicate substantial contribution of asthenospheric material in the Malani melting process.
DOI: 10.6084/m9.figshare.14535512.v1
title: Neoproterozoic geodynamics in NW India – evidence from Erinpura granites in the South Delhi Fold Belt

description: Erinpura Granites form the basement for the Neoproterozoic Malani Igneous Suite in NW India. Based on this study, the Erinpura granites can be divided into Erinpura-East (gneissic fabric), a belt parallel to the southern sector of the South Delhi Fold Belt, and Erinpura-West (magmatic fabrics). EPMA dating on monazites gives a time frame of 890 to 860 Ma for crystallization of both types. The geochemically homogeneous peraluminous S-type granites with ε<sub>Nd</sub> values of −2.1 to −10.8 are interpreted as melting products of Archaean crust. REE pattern follows the pattern of the average continental crust, but Erinpura-East samples are more fractionated with steeper HREE depletion indicating melting in a deeper crustal level. A thermal pulse between 835 and 820 Ma constrains the timing of deformation in granite-gneisses during uplift along thrust planes, coeval with shear-bound exhumation of high-grade metamorphic rocks and initiated by delamination of the lower crust in this southern sector of the South Delhi Fold Belt. This is in contrast to the northern sector of the SDFB with arrested orogenic development and without considerable delamination or erosion of the lower crust. Latest movement related to the 200 Ma tectono-magmatic history overlaps with initiation of rifting during the Malani igneous event. A change from S-type to A-type granites and shift of isotopic signatures to ε<sub>Nd</sub> values of −2.8 to −1.7 indicate substantial contribution of asthenospheric material in the Malani melting process.
DOI: 10.6084/m9.figshare.14632608
title: Late Ediacaran post-collisional magmatism in the Guéra Massif, South-Central Chad

description: The Guéra Massif of South-Central Chad is composed of collisional and post-collisional intrusive rocks related to the Central African Orogenic Belt. Collisional granites were emplaced at 595–590 Ma but there are a series of post-collisional intrusions that were emplaced at 570–560 Ma. The older granites have zircon U-Pb weighted-mean ages of 569 ± 6 Ma, 568 ± 7 Ma, and 568 ± 6 Ma, whereas the younger granites are 556 ± 7 Ma and 561 ± 6 Ma but all ages are within their maximum uncertainty. Both groups of post-collisional granites are peraluminous, ferroan, and alkali calcic to calc-alkalic but dioritic microgranular enclaves were observed within the older granites. The chemical variability of each group can be explained by fractional crystallization and it is likely that their parental magmas were derived by partial melting of the lower crust. The Nd isotopes of the older rocks (ε<sub>Nd</sub>(<i>t</i>) = −9.5 to −1.2) are slightly less enriched than the younger rocks (ε<sub>Nd</sub>(<i>t)</i> = −13.1 and −9.1). Moreover, the Nd isotopic compositions appear to indicate the existence of two isotopically distinct regions of the Guéra Massif with one centred on the Mongo (west) region and the other near the El Hidjer to Zan (east) region. The older group was emplaced during a period of crustal thinning after oblique collision and shearing related to the final suturing of the Congo-Saõ Francisco Craton and the Saharan Metacraton. The younger group was likely emplaced after a period of regional WNW-ESE directed crustal shortening. The punctuated nature of deformation/crustal relaxation cycles in the southern Saharan Metacraton suggests that there may have been many small terranes rather than larger cratonic blocks involved in the lithotectonic evolution of the Central African Orogenic Belt north of the Congo-Saõ Francisco Craton.
DOI: 10.6084/m9.figshare.14371301
title: Tectonic significance of the late Eocene (Bartonian) calc-alkaline granitoid body in the Marivan area, Zagros suture zone, northwest Iran

description: The Marivan granitoid body of the northern Sanandaj–Sirjan Zone (N-SaSZ) of northwest Iran was emplaced into Cretaceous sediments, and is associated with minor amounts of iron skarn-type mineralization along the contact between the intrusion and surrounding country rocks. The granitoids within the intrusion include (hornblende-rich) diorite, granodiorite, and granite phases, and zircon U–Pb dating of four samples from this intrusion indicate they were emplaced during the late Eocene (Bartonian; 37.7 ± 1.0 Ma). These plutonic rocks can be classified into two main types, granitic and dioritic rocks, according to petrography and whole-rock major element geochemistry. Both the granitic and dioritic rocks are high-K, and some of the granitic rocks have an I-type affinity and peraluminous to metaluminous compositions. Both the granitic and dioritic rocks have ε<sub>Nd</sub>(t) values that cluster around zero (–3.3 to +3.0) and low <sup>87</sup>Sr/<sup>86</sup>Sr<sub>(i)</sub> values (0.7040–0.7076), suggesting derivation from a mafic juvenile crustal or depleted mantle source, which was possibly mafic calc-alkaline rocks or amphibolites within the lower crust. The new zircon U–Pb ages and petrological and geochemical data presented in this study suggest that the Palaeocene–early Eocene collision of the Arabian and Iranian plates caused the ascent and emplacement of hot mafic magma through a slab window into the crust. This increased the geothermal gradient within the root zone of the developing magmatic system at the base of the continental crust, causing the partial melting of lower crust in this region. This generated mafic to intermediate magmas that were either directly emplaced into the upper crust or mixed with varying amounts of upper crustal material prior to emplacement, which formed the diorite to leucogranite range of compositions within the Marivan granitoid intrusion.
DOI: 10.6084/m9.figshare.14632608.v1
title: Late Ediacaran post-collisional magmatism in the Guéra Massif, South-Central Chad

description: The Guéra Massif of South-Central Chad is composed of collisional and post-collisional intrusive rocks related to the Central African Orogenic Belt. Collisional granites were emplaced at 595–590 Ma but there are a series of post-collisional intrusions that were emplaced at 570–560 Ma. The older granites have zircon U-Pb weighted-mean ages of 569 ± 6 Ma, 568 ± 7 Ma, and 568 ± 6 Ma, whereas the younger granites are 556 ± 7 Ma and 561 ± 6 Ma but all ages are within their maximum uncertainty. Both groups of post-collisional granites are peraluminous, ferroan, and alkali calcic to calc-alkalic but dioritic microgranular enclaves were observed within the older granites. The chemical variability of each group can be explained by fractional crystallization and it is likely that their parental magmas were derived by partial melting of the lower crust. The Nd isotopes of the older rocks (ε<sub>Nd</sub>(<i>t</i>) = −9.5 to −1.2) are slightly less enriched than the younger rocks (ε<sub>Nd</sub>(<i>t)</i> = −13.1 and −9.1). Moreover, the Nd isotopic compositions appear to indicate the existence of two isotopically distinct regions of the Guéra Massif with one centred on the Mongo (west) region and the other near the El Hidjer to Zan (east) region. The older group was emplaced during a period of crustal thinning after oblique collision and shearing related to the final suturing of the Congo-Saõ Francisco Craton and the Saharan Metacraton. The younger group was likely emplaced after a period of regional WNW-ESE directed crustal shortening. The punctuated nature of deformation/crustal relaxation cycles in the southern Saharan Metacraton suggests that there may have been many small terranes rather than larger cratonic blocks involved in the lithotectonic evolution of the Central African Orogenic Belt north of the Congo-Saõ Francisco Craton.
DOI: 10.6084/m9.figshare.17128452
title: Role of Late Cretaceous volcanic-sedimentary melanges, specifically the Aladağ melange, E Turkey, in the rift-drift-subduction-accretion-emplacement history of the Tethyan Inner Tauride ocean

description: The Aladağ melange is located between Mesozoic Tauride carbonate platform units and the Late Cretaceous Pozantı-Karsantı ophiolite and its metamorphic sole. The melange comprises a lower, mainly sedimentary unit, composed of variably disrupted thrust sheets of deep-sea sediments, with a localized matrix of mass-flow and turbidity current deposits. The upper, volcanic-sedimentary melange comprises highly disrupted basalt-pelagic carbonate-radiolarite units, rarely associated with gravity-flow deposits. Tholeiitic to alkaline basalts in the melange range from N-MORB, to E-MORB and to OIB, and are dated as Middle Jurassic to Early Cretaceous using Radiolaria from interbedded pelagic sediments. Comparisons with accretionary melanges throughout southern Turkey and elsewhere indicate a similar geochemical pattern of variable ‘enrichment’, commonly coupled with a subduction influence (e.g. negative Nb, Ta anomalies). Geochemically, the subduction-influenced basalts are consistent with an oceanic island arc origin. However, the geological setting of Triassic basalts within some of the melanges (e.g. Mersin) is indicative of a rifted continental margin setting. The Mesozoic basalts within the Turkish melanges considered here erupted along the distal, outer northern margin of the Tauride continent, followed by Late Cretaceous subduction-accretion and supra-subduction zone ophiolite emplacement. Regional to global chemical comparisons suggest that the subduction influence could represent geochemical subduction inheritance rather than contemporaneous subduction.
DOI: 10.6084/m9.figshare.14371301.v1
title: Tectonic significance of the late Eocene (Bartonian) calc-alkaline granitoid body in the Marivan area, Zagros suture zone, northwest Iran

description: The Marivan granitoid body of the northern Sanandaj–Sirjan Zone (N-SaSZ) of northwest Iran was emplaced into Cretaceous sediments, and is associated with minor amounts of iron skarn-type mineralization along the contact between the intrusion and surrounding country rocks. The granitoids within the intrusion include (hornblende-rich) diorite, granodiorite, and granite phases, and zircon U–Pb dating of four samples from this intrusion indicate they were emplaced during the late Eocene (Bartonian; 37.7 ± 1.0 Ma). These plutonic rocks can be classified into two main types, granitic and dioritic rocks, according to petrography and whole-rock major element geochemistry. Both the granitic and dioritic rocks are high-K, and some of the granitic rocks have an I-type affinity and peraluminous to metaluminous compositions. Both the granitic and dioritic rocks have ε<sub>Nd</sub>(t) values that cluster around zero (–3.3 to +3.0) and low <sup>87</sup>Sr/<sup>86</sup>Sr<sub>(i)</sub> values (0.7040–0.7076), suggesting derivation from a mafic juvenile crustal or depleted mantle source, which was possibly mafic calc-alkaline rocks or amphibolites within the lower crust. The new zircon U–Pb ages and petrological and geochemical data presented in this study suggest that the Palaeocene–early Eocene collision of the Arabian and Iranian plates caused the ascent and emplacement of hot mafic magma through a slab window into the crust. This increased the geothermal gradient within the root zone of the developing magmatic system at the base of the continental crust, causing the partial melting of lower crust in this region. This generated mafic to intermediate magmas that were either directly emplaced into the upper crust or mixed with varying amounts of upper crustal material prior to emplacement, which formed the diorite to leucogranite range of compositions within the Marivan granitoid intrusion.
DOI: 10.48370/ofd/gmnscm
title: Plagionotus floralis (Pallas, 1773), C-859

description: Coleoptera collection
DOI: 10.5519/qd.bv6rwp6d
title: Query on the Natural History Museum Data Portal (data.nhm.ac.uk) (1 records)
DOI: 10.21942/uva.16929505.v1
title: Dataset belonging to Siebers et al. (2021) Social Media Are a Powerful Distractor for the Vast Majority of Adolescents

description: The codebook, preregistration, syntaxes, and online supplemental materials can be found on the Open Science Framework (OSF) at https://osf.io/54uzf/.<br>For more information, please contact the authors via t.siebers@uva.nl or info@project-awesome.nl.
DOI: 10.48370/ofd/fsga8c
title: Plagionotus scalaris (Brullé, 1832), C-860

description: Coleoptera collection
DOI: 10.48370/ofd/n6lxap/lj45iw
title: Plagionotus lugubris.JPG

description: :unav
DOI: 10.48370/ofd/n6lxap
title: Plagionotus lugubris (Ménétriés, 1832), C-861

description: Coleoptera collection
DOI: 10.4119/unibi/2960835
title: Dataset for "The Chiral Phase Transition in 3-flavor QCD from Lattice QCD"

description: Data publication with data to reproduce all figures in "The Chiral Phase Transition in 3-flavor QCD from Lattice QCD", [Phys.Rev.D 105 (2022) 3, 034510](https://journals.aps.org/prd/abstract/10.1103/PhysRevD.105.034510), [arXiv:2111.12599](https://arxiv.org/abs/2111.12599).
DOI: 10.48370/ofd/yqj8ev
title: Plagionotus lugubris (Ménétriés, 1832), C-862

description: Coleoptera collection
DOI: 10.21227/5w3x-5525
title: Image-grade LiDAR dataset

description: This dataset provides a dataset of high resolution image-grade LiDAR SLAM in .bag format.
DOI: 10.48370/ofd/rbuhth
title: Plagionotus bobelayi (Brullé, 1832), C-863

description: Coleoptera collection
DOI: 10.6084/m9.figshare.19612977
title: original data.xlsx

description: soil total PLFA (Total), fungi (F), bacteria (B), F/B, Gram-positive bacterial (GP), Gram-negative bacterial (GN), the ratio of Gram-positive bacterial to Gram-negative bacterial (GP/GN ), arbuscular mycorrhizal fungi (AMF) and soil water content (SWC), pH, total carbon (TC), total nitrogen (TN), available nitrogen (AN), dissolved organic carbon (DOC), microbial biomass carbon (MBC), microbial biomass nitrogen (MBN) in control and clipping treatments of <em>Agropyron cristatum</em> (Ac), <em>Stipa krylovii</em> (Sk), <em>Potentilla tanacetifolia </em>(Pt), <em>Artemisia frigida</em> (Af), <em>Lespedeza davurica</em> (Ld), <em>Leymus chinensis</em> (Lc) sites
DOI: 10.6084/m9.figshare.19612977.v1
title: original data.xlsx

description: soil total PLFA (Total), fungi (F), bacteria (B), F/B, Gram-positive bacterial (GP), Gram-negative bacterial (GN), the ratio of Gram-positive bacterial to Gram-negative bacterial (GP/GN ), arbuscular mycorrhizal fungi (AMF) and soil water content (SWC), pH, total carbon (TC), total nitrogen (TN), available nitrogen (AN), dissolved organic carbon (DOC), microbial biomass carbon (MBC), microbial biomass nitrogen (MBN) in control and clipping treatments of <em>Agropyron cristatum</em> (Ac), <em>Stipa krylovii</em> (Sk), <em>Potentilla tanacetifolia </em>(Pt), <em>Artemisia frigida</em> (Af), <em>Lespedeza davurica</em> (Ld), <em>Leymus chinensis</em> (Lc) sites
DOI: 10.6084/m9.figshare.19613608.v1
title: Additional file 1 of Planning a method for covariate adjustment in individually randomised trials: a practical guide

description: Additional file 1 Stata code to generate Fig. 1.
DOI: 10.6084/m9.figshare.19613611
title: Additional file 2 of Planning a method for covariate adjustment in individually randomised trials: a practical guide

description: Additional file 2 Stata code for the analysis of the GetTested trial (Assumes the data file journal.pmed.1002479.s001.xls has been downloaded from https://journals.plos.org/plosmedicine/article?id=10.1371/journal.pmed.1002479#sec020 ).
DOI: 10.6084/m9.figshare.19613611.v1
title: Additional file 2 of Planning a method for covariate adjustment in individually randomised trials: a practical guide

description: Additional file 2 Stata code for the analysis of the GetTested trial (Assumes the data file journal.pmed.1002479.s001.xls has been downloaded from https://journals.plos.org/plosmedicine/article?id=10.1371/journal.pmed.1002479#sec020 ).
DOI: 10.6084/m9.figshare.19613608
title: Additional file 1 of Planning a method for covariate adjustment in individually randomised trials: a practical guide

description: Additional file 1 Stata code to generate Fig. 1.
DOI: 10.6084/m9.figshare.19613644
title: Additional file 3 of Utilization of provider-initiated HIV testing and counselling in Ethiopia: a systematic review and meta-analysis

description: Additional file 3. Risk of bias assessment of studies included for systematic review and meta-analysis on utilization of PITC in Ethiopia.
DOI: 10.6084/m9.figshare.19613644.v1
title: Additional file 3 of Utilization of provider-initiated HIV testing and counselling in Ethiopia: a systematic review and meta-analysis

description: Additional file 3. Risk of bias assessment of studies included for systematic review and meta-analysis on utilization of PITC in Ethiopia.
DOI: 10.6084/m9.figshare.19613698
title: Additional file 15 of An alternative CYB5A transcript is expressed in aneuploid ALL and enriched in relapse

description: Additional file 15. Genetic alterations in relapsed NH/HeH BCP-ALL patients (n = 10). The table summarises the number of genetic events occurring in NH/HeH BCP-ALL patients (n = 10) in cohort 1 as assessed by Exonseq and gene panel sequencing. Sheet 1 (summary) summarises recurrent genetic alterations (count &gt; 1), subdivided into gene mutations (mutational count, detected by Exonseq and panel sequencing) and copy number alterations (CNA count, Exonseq). Sheet 2 (mutations) and sheet 3 (can) list all detected genetic alterations in relapsed NH / HeH BCP-ALL patients.