cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.5517/ccdc.csd.cc2fbjq1
title: CCDC 2244453: Experimental Crystal Structure Determination

description: Related Article: H. Yuan, R. Zhang, K. Hu, R. Fang|2023|Acta Crystallogr.,Sect.C:Cryst.Struct.Chem.|79|193|doi:10.1107/S2053229623003388
description: An entry from the Cambridge Structural Database, the world’s repository for small molecule crystal structures. The entry contains experimental data from a crystal diffraction study. The deposited dataset for this entry is freely available from the CCDC and typically includes 3D coordinates, cell parameters, space group, experimental conditions and quality measures.
DOI: 10.6084/m9.figshare.22123666.v1
title: Petrogenesis of the Kalka, Ewarara and Gosse Pile layered intrusions, Musgrave Province, South Australia, and implications for magmatic sulfide prospectivity

description: The Musgrave Province of central Australia was the focus of long-lived mantle upwelling that produced large volumes of magnesian basaltic to tholeiitic magma and their felsic derivatives. The Musgrave Province contains one of the greatest concentrations of mafic–ultramafic layered intrusions globally, grouped as the Giles intrusions. In the present paper, we study the magmatic ore potential of the Kalka, Gosse Pile and Ewarara layered intrusions located in South Australia. Ewarara and Gosse Pile appear to have relatively low potential for platnium-group element (PGE) reefs and magmatic Ni–Cu, based on lack of evident metal enrichment and the absence of a mafic–ultramafic transition zone that hosts most PGE reefs globally. However, mafic–ultramafic pipes within the intrusions that could have higher ore potential have not been studied by us. At Kalka, the mafic–ultramafic transition interval is exposed, rendering this intrusion potentially more prospective for PGE reefs. However, based on the available data, this zone appears to be barren. Instead, there are signs of PGE enrichment and metal ratio variation in the magnetite-bearing upper portion of the intrusion suggestive of undiscovered PGE reefs. This interpretation is consistent with subtle Cu–Pd enrichment of soils adjacent to the upper portion of the intrusion.KEY POINTSFirst assessment of magmatic ore potential of Kalka, Ewarara and Gosse Pile layered intrusions in South Australia.Kalka shows signs of PGE enrichment in upper, magnetite-bearing portion of intrusion, suggesting enhanced potential for a PGE reef.Ewarara and Gosse Pile appear to be less prospective for PGE–Ni–Cu, but picrite pipes remain unstudied. First assessment of magmatic ore potential of Kalka, Ewarara and Gosse Pile layered intrusions in South Australia. Kalka shows signs of PGE enrichment in upper, magnetite-bearing portion of intrusion, suggesting enhanced potential for a PGE reef. Ewarara and Gosse Pile appear to be less prospective for PGE–Ni–Cu, but picrite pipes remain unstudied.
DOI: 10.6084/m9.figshare.22123666
title: Petrogenesis of the Kalka, Ewarara and Gosse Pile layered intrusions, Musgrave Province, South Australia, and implications for magmatic sulfide prospectivity

description: The Musgrave Province of central Australia was the focus of long-lived mantle upwelling that produced large volumes of magnesian basaltic to tholeiitic magma and their felsic derivatives. The Musgrave Province contains one of the greatest concentrations of mafic–ultramafic layered intrusions globally, grouped as the Giles intrusions. In the present paper, we study the magmatic ore potential of the Kalka, Gosse Pile and Ewarara layered intrusions located in South Australia. Ewarara and Gosse Pile appear to have relatively low potential for platnium-group element (PGE) reefs and magmatic Ni–Cu, based on lack of evident metal enrichment and the absence of a mafic–ultramafic transition zone that hosts most PGE reefs globally. However, mafic–ultramafic pipes within the intrusions that could have higher ore potential have not been studied by us. At Kalka, the mafic–ultramafic transition interval is exposed, rendering this intrusion potentially more prospective for PGE reefs. However, based on the available data, this zone appears to be barren. Instead, there are signs of PGE enrichment and metal ratio variation in the magnetite-bearing upper portion of the intrusion suggestive of undiscovered PGE reefs. This interpretation is consistent with subtle Cu–Pd enrichment of soils adjacent to the upper portion of the intrusion.KEY POINTSFirst assessment of magmatic ore potential of Kalka, Ewarara and Gosse Pile layered intrusions in South Australia.Kalka shows signs of PGE enrichment in upper, magnetite-bearing portion of intrusion, suggesting enhanced potential for a PGE reef.Ewarara and Gosse Pile appear to be less prospective for PGE–Ni–Cu, but picrite pipes remain unstudied. First assessment of magmatic ore potential of Kalka, Ewarara and Gosse Pile layered intrusions in South Australia. Kalka shows signs of PGE enrichment in upper, magnetite-bearing portion of intrusion, suggesting enhanced potential for a PGE reef. Ewarara and Gosse Pile appear to be less prospective for PGE–Ni–Cu, but picrite pipes remain unstudied.
DOI: 10.6084/m9.figshare.22321130
title: Early Permian zircon ages from the <i>P. confluens</i> and <i>P. pseudoreticulata</i> spore-pollen zones in the southern Bonaparte and Canning basins, northwestern Australia

description: The <i>Pseudoreticulatispora confluens–P. pseudoreticulata</i> spore-pollen zonal datum typically coincides with the end of widespread Permian glacial deposits in Western Australia. Although previously attributed to the mid-Sakmarian, chemical abrasion isotope dilution thermal ionisation mass spectrometry (TIMS) dating of zircons from volcanic tuffs in the Ditji Formation of the Bonaparte Basin and the Grant Group in the Canning Basin point to an Asselian age of about 295.25 Ma for this datum. All dated zircons from the Ditji Formation came from petroleum well cuttings but the accompanying palynology was mostly from sidewall cores; however, all Grant Group samples were from conventional core. TIMS dates from the Ditji Formation range in age from 295.2 to 292.7 Ma whereas the only productive tuff from the Grant Group yielded a 296.26 Ma date. By comparison, there are no zircon dates to constrain the onset of glacial deposition in Australia. The Bonaparte Basin ages overlap with those for the Edie Tuff (296.1–294.5 Ma) in Queensland’s Galilee Basin, approximately 2000 km to the southeast, which also lies close to the base of the <i>P. pseudoreticulata</i> Zone. To date the only fossil group within the <i>P. confluens</i> Zone in Western Australia to provide independent age control, albeit loosely, are goniatites from the northern Perth Basin (<i>Uraloceras irwinense</i> and <i>Juresanites jacksoni)</i> that have consistently been attributed to the Sakmarian; these require a reassessment of their affinity with Russian faunas and therefore to global stratotypes. The position of the Carboniferous–Permian boundary is elusive in Australia and will remain so until additional volcanic tuffs containing young datable zircons are found; however, spore-pollen and zircon dates from Namibia place this boundary within the <i>P. confluens</i> Zone.
DOI: 10.6084/m9.figshare.22114702
title: Petrogenesis and tectonic setting of Early Cretaceous mafic dykes in the North Qinling Orogenic Belt, central China: constraints on the lithospheric lower crust delamination

description: Late Mesozoic mafic dykes, which are widely developed in the North Qinling Orogenic Belt (NQOB), include abundant geodynamic information. This paper describes the mafic dykes that intrude the Late Jurassic granite in the Dayu and Kuyu areas, and reports important petrological constraints for the late Mesozoic tectonic transition from compression to extension in the NQOB. Three zircon U–Pb results show that the minimum ages of the mafic dykes are 139.8 ± 1.4 Ma, 137.4 ± 1.7 Ma and 133.4 ± 0.9 Ma, indicating that the emplacement age of the Dayu and Kuyu mafic dykes is 140–133 Ma. Petrogeochemical analyses suggest that the mafic dykes belong to the high-K calc-alkaline shoshonite series with low SiO<sub>2</sub> (46.93–56.73 wt%), MgO (1.88–9.10 wt%) and TiO<sub>2</sub> (1.17–1.82 wt%), and high Al<sub>2</sub>O<sub>3</sub> (13.98–17.46 wt%), TFe<sub>2</sub>O<sub>3</sub> (7.81–10.92 wt%) and K<sub>2</sub>O (1.28–4.78 wt%). The mafic dykes are enriched in large ion lithophile elements (<i>e.g.</i> Rb, Ba, K, La, Sr) and depleted in high-field-strength elements (<i>e.g.</i> Nb, Ta, Zr, Ti). These samples have the right-sloping chondrite-normalised rare earth element patterns, which suggest light rare earth element enrichment and heavy rare earth elements depletion with no obvious Eu anomalies (δEu = 0.94–1.11). The <i>I</i><sub>Sr</sub>, <i>ε</i><sub>Nd</sub>(t), <i>ε</i><sub>Hf</sub> (t) and <i>T</i><sub>DM2(crust)</sub> values are 0.7056–0.7060, −10.60 to −5.98, −14.1 to −2.8, and 1382.4 ± 25.1 to 2081.9 ± 47.6 Ma, respectively. Both elemental and isotopic geochemistry show that the formation of Dayu and Kuyu mafic dykes is due to the partial decompression melting of previously enriched lithospheric mantle during a delamination process. The mafic dykes have undergone fractionation crystallisation of Mg–Fe phase minerals during magma ascent, accompanied by some crustal contamination. Combined with the regional tectonic setting, we suggested that the NQOB experienced intra-continental extension during the Early Cretaceous.KEY POINTSEarly Cretaceous (140–133 Ma) mafic dykes have been discovered in the middle part of the North Qinling Orogenic Belt.The remote effect of the Paleo-Pacific Plate subduction has reached the middle of the North Qinling Orogenic Belt.The North Qinling Orogenic Belt entered the extensional stage in the Early Cretaceous (140–133 Ma). Early Cretaceous (140–133 Ma) mafic dykes have been discovered in the middle part of the North Qinling Orogenic Belt. The remote effect of the Paleo-Pacific Plate subduction has reached the middle of the North Qinling Orogenic Belt. The North Qinling Orogenic Belt entered the extensional stage in the Early Cretaceous (140–133 Ma).
DOI: 10.6084/m9.figshare.22114702.v1
title: Petrogenesis and tectonic setting of Early Cretaceous mafic dykes in the North Qinling Orogenic Belt, central China: constraints on the lithospheric lower crust delamination

description: Late Mesozoic mafic dykes, which are widely developed in the North Qinling Orogenic Belt (NQOB), include abundant geodynamic information. This paper describes the mafic dykes that intrude the Late Jurassic granite in the Dayu and Kuyu areas, and reports important petrological constraints for the late Mesozoic tectonic transition from compression to extension in the NQOB. Three zircon U–Pb results show that the minimum ages of the mafic dykes are 139.8 ± 1.4 Ma, 137.4 ± 1.7 Ma and 133.4 ± 0.9 Ma, indicating that the emplacement age of the Dayu and Kuyu mafic dykes is 140–133 Ma. Petrogeochemical analyses suggest that the mafic dykes belong to the high-K calc-alkaline shoshonite series with low SiO<sub>2</sub> (46.93–56.73 wt%), MgO (1.88–9.10 wt%) and TiO<sub>2</sub> (1.17–1.82 wt%), and high Al<sub>2</sub>O<sub>3</sub> (13.98–17.46 wt%), TFe<sub>2</sub>O<sub>3</sub> (7.81–10.92 wt%) and K<sub>2</sub>O (1.28–4.78 wt%). The mafic dykes are enriched in large ion lithophile elements (<i>e.g.</i> Rb, Ba, K, La, Sr) and depleted in high-field-strength elements (<i>e.g.</i> Nb, Ta, Zr, Ti). These samples have the right-sloping chondrite-normalised rare earth element patterns, which suggest light rare earth element enrichment and heavy rare earth elements depletion with no obvious Eu anomalies (δEu = 0.94–1.11). The <i>I</i><sub>Sr</sub>, <i>ε</i><sub>Nd</sub>(t), <i>ε</i><sub>Hf</sub> (t) and <i>T</i><sub>DM2(crust)</sub> values are 0.7056–0.7060, −10.60 to −5.98, −14.1 to −2.8, and 1382.4 ± 25.1 to 2081.9 ± 47.6 Ma, respectively. Both elemental and isotopic geochemistry show that the formation of Dayu and Kuyu mafic dykes is due to the partial decompression melting of previously enriched lithospheric mantle during a delamination process. The mafic dykes have undergone fractionation crystallisation of Mg–Fe phase minerals during magma ascent, accompanied by some crustal contamination. Combined with the regional tectonic setting, we suggested that the NQOB experienced intra-continental extension during the Early Cretaceous.KEY POINTSEarly Cretaceous (140–133 Ma) mafic dykes have been discovered in the middle part of the North Qinling Orogenic Belt.The remote effect of the Paleo-Pacific Plate subduction has reached the middle of the North Qinling Orogenic Belt.The North Qinling Orogenic Belt entered the extensional stage in the Early Cretaceous (140–133 Ma). Early Cretaceous (140–133 Ma) mafic dykes have been discovered in the middle part of the North Qinling Orogenic Belt. The remote effect of the Paleo-Pacific Plate subduction has reached the middle of the North Qinling Orogenic Belt. The North Qinling Orogenic Belt entered the extensional stage in the Early Cretaceous (140–133 Ma).
DOI: 10.6084/m9.figshare.22321130.v2
title: Early Permian zircon ages from the <i>P. confluens</i> and <i>P. pseudoreticulata</i> spore-pollen zones in the southern Bonaparte and Canning basins, northwestern Australia

description: The <i>Pseudoreticulatispora confluens–P. pseudoreticulata</i> spore-pollen zonal datum typically coincides with the end of widespread Permian glacial deposits in Western Australia. Although previously attributed to the mid-Sakmarian, chemical abrasion isotope dilution thermal ionisation mass spectrometry (TIMS) dating of zircons from volcanic tuffs in the Ditji Formation of the Bonaparte Basin and the Grant Group in the Canning Basin point to an Asselian age of about 295.25 Ma for this datum. All dated zircons from the Ditji Formation came from petroleum well cuttings but the accompanying palynology was mostly from sidewall cores; however, all Grant Group samples were from conventional core. TIMS dates from the Ditji Formation range in age from 295.2 to 292.7 Ma whereas the only productive tuff from the Grant Group yielded a 296.26 Ma date. By comparison, there are no zircon dates to constrain the onset of glacial deposition in Australia. The Bonaparte Basin ages overlap with those for the Edie Tuff (296.1–294.5 Ma) in Queensland’s Galilee Basin, approximately 2000 km to the southeast, which also lies close to the base of the <i>P. pseudoreticulata</i> Zone. To date the only fossil group within the <i>P. confluens</i> Zone in Western Australia to provide independent age control, albeit loosely, are goniatites from the northern Perth Basin (<i>Uraloceras irwinense</i> and <i>Juresanites jacksoni)</i> that have consistently been attributed to the Sakmarian; these require a reassessment of their affinity with Russian faunas and therefore to global stratotypes. The position of the Carboniferous–Permian boundary is elusive in Australia and will remain so until additional volcanic tuffs containing young datable zircons are found; however, spore-pollen and zircon dates from Namibia place this boundary within the <i>P. confluens</i> Zone.
DOI: 10.6084/m9.figshare.22321130.v1
title: Early Permian zircon ages from the <i>P. confluens</i> and <i>P. pseudoreticulata</i> spore-pollen zones in the southern Bonaparte and Canning basins, Northwestern Australia

description: The <i>Pseudoreticulatispora confluens–P. pseudoreticulata</i> spore-pollen zonal datum typically coincides with the end of widespread Permian glacial deposits in Western Australia. Although previously attributed to the mid-Sakmarian, chemical abrasion isotope dilution thermal ionisation mass spectrometry (TIMS) dating of zircons from volcanic tuffs in the Ditji Formation of the Bonaparte Basin and the Grant Group in the Canning Basin point to an Asselian age of about 295.25 Ma for this datum. All dated zircons from the Ditji Formation came from petroleum well cuttings but the accompanying palynology was mostly from sidewall cores; however, all Grant Group samples were from conventional core. TIMS dates from the Ditji Formation range in age from 295.2 to 292.7 Ma whereas the only productive tuff from the Grant Group yielded a 296.26 Ma date. By comparison, there are no zircon dates to constrain the onset of glacial deposition in Australia. The Bonaparte Basin ages overlap with those for the Edie Tuff (296.1–294.5 Ma) in Queensland’s Galilee Basin, approximately 2000 km to the southeast, which also lies close to the base of the <i>P. pseudoreticulata</i> Zone. To date the only fossil group within the <i>P. confluens</i> Zone in Western Australia to provide independent age control, albeit loosely, are goniatites from the northern Perth Basin (<i>Uraloceras irwinense</i> and <i>Juresanites jacksoni)</i> that have consistently been attributed to the Sakmarian; these require a reassessment of their affinity with Russian faunas and therefore to global stratotypes. The position of the Carboniferous–Permian boundary is elusive in Australia and will remain so until additional volcanic tuffs containing young datable zircons are found; however, spore-pollen and zircon dates from Namibia place this boundary within the <i>P. confluens</i> Zone.
DOI: 10.3886/e183611v2-138600
title: Governments' Economic Responses to COVID-19 (Econ-Response2covid19)

description: We introduce a new dataset of ten economic measures in percentage of gross domestic product implemented by governments worldwide between January 2020 and June 2021 to fight COVID-19. The measures coded include fiscal measures (wage support, cash transfers, in-kind transfers, tax cuts, sectorial support and credit schemes), tax deferrals, off-budget measures, and main policy rate cuts. The data can be used to study the impact of economic measures on different outcomes, and to understand the diffusion of economic policies during crises.
description: Presence of Common Scales: Measures are coded in % of 2019 GDP.
description: Smallest Geographic Unit: Country or territory
description: other;
DOI: 10.6084/m9.figshare.22799981
title: Additional file 2 of Linear accelerator-based stereotactic radiotherapy for brain metastases, including multiple and large lesions, carries a low incidence of acute toxicities: a retrospective analysis

description: Additional file 2: Table S1. Characteristics of all patients who experienced immediate side effects.
DOI: 10.6084/m9.figshare.22799981.v1
title: Additional file 2 of Linear accelerator-based stereotactic radiotherapy for brain metastases, including multiple and large lesions, carries a low incidence of acute toxicities: a retrospective analysis

description: Additional file 2: Table S1. Characteristics of all patients who experienced immediate side effects.
DOI: 10.6084/m9.figshare.22800029
title: Additional file 3 of Expression of L1 retrotransposons in granulocytes from patients with active systemic lupus erythematosus

description: Additional file 3: Supplemental Table 1. Individual uniquely mapping read counts of the 7 L1 elements expressed at elevated levels in SLE patients.
DOI: 10.6084/m9.figshare.22800029.v1
title: Additional file 3 of Expression of L1 retrotransposons in granulocytes from patients with active systemic lupus erythematosus

description: Additional file 3: Supplemental Table 1. Individual uniquely mapping read counts of the 7 L1 elements expressed at elevated levels in SLE patients.
DOI: 10.6084/m9.figshare.22799912.v1
title: 新建 Microsoft Excel 工作表.xlsx

description: test
DOI: 10.6084/m9.figshare.22799912
title: test2

description: test
DOI: 10.6084/m9.figshare.22799912.v2
title: 新建 Microsoft Excel 工作表.xlsx

description: test
DOI: 10.6084/m9.figshare.22799912.v3
title: test2

description: test
DOI: 10.25919/5z99-h749
title: Annual vegetation height images for Australia from GEDI and Landsat data

description: An Australia-wide vegetation height was generated using Global Ecosystem Dynamics Investigation (GEDI) LiDAR Altimetry (from 2019) and used to train a random forest model to provide vegetation height from Landsat data available in Digital Earth Australia. The Landsat data used for extrapolating vegetation height images were the Annual Fractional Cover product and the Annual Geomedian product. The random forest model was used to generate annual vegetation height from 1988 to 2021. To reduce errors in irrigated agriculture, vegetation height below three metres was set to zero. Refer to the metadata for a description of the method and validation of this product and the Readme.txt for the data format (see Supporting files). This method was developed through the CSIRO Digiscape Future Science Platform and updated as part of the Regional Land and Ecosystem Accounts project, which is funded through the Australian Department of Climate Change, Energy the Environment and Water (DCCEEW).
DOI: 10.25901/w3z2-z817
title: Calperum Mallee Site, Monthly Rainfall Data 1995-2011, Calperum Station
DOI: 10.7934/x29045
title: REVISION OF CHINESE CAPTORHINIDS [X29045] Captorhinid interrelationships
DOI: 10.5281/zenodo.7853082
title: Predicting Pulsed Laser Deposition SrTiO3 Homoepitaxy Growth Dynamics using High-Speed Reflection High-Energy Electron Diffraction - sample treated_81nm

description: RHEED intensity image dataset of sample <strong>t0.08</strong> in work "Predicting Pulsed Laser Deposition SrTiO<sub>3 </sub>Homoepitaxy Growth Dynamics using High-Speed Reflection High-Energy Electron Diffraction."
DOI: 10.5281/zenodo.7853081
title: Predicting Pulsed Laser Deposition SrTiO3 Homoepitaxy Growth Dynamics using High-Speed Reflection High-Energy Electron Diffraction - sample treated_81nm

description: RHEED intensity image dataset of sample <strong>t0.08</strong> in work "Predicting Pulsed Laser Deposition SrTiO<sub>3 </sub>Homoepitaxy Growth Dynamics using High-Speed Reflection High-Energy Electron Diffraction."
DOI: 10.3886/e118302v1-138601
title: Data and Code for: The Extensive Margin of Exporting Products: A Firm-level Analysis

description: Abstract:<br><br> To quantify trade frictions, we examine multi-product exporters. We build a flexible general- equilibrium model and estimate market entry costs using Brazilian firm-product-destination data under rich demand and market-access cost shocks. Our estimates show that additional products farther from a firm’s core competency come at higher production costs, but there are substantive economies of scope in market-access costs. Market-access costs differ across destinations, falling more rapidly in nearby regions and at destinations with fewer non-tariff barriers. We evaluate a counterfactual scenario that harmonizes market-access costs across destinations and find global welfare gains similar to eliminating all current tariffs. <br>
description: Response Rates: Administrative data collected by customs authorities.
description: All Brazilian Manufacturing Exporters. Smallest Geographic Unit: Brazil
description: The paper uses confidential employer-employee data from RAIS, Brazil. We were given access to these data under the agreement that they could not be made publicly available. Raw data access is available at IPEA Brasilia and IBGE Rio de Janeiro. We will make available our code and hold the final estimation data ready for replication purposes.
DOI: 10.6084/m9.figshare.22785491
title: Classification of MLH1 missense VUS using protein structure-based deep learning-Ramachandran plot-molecular dynamics simulations method

description: Variant of Uncertain Significance Ramchandran Scatter Plot files in CSV format