cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.5517/ccdc.csd.cc11336g
title: CCDC 956294: Experimental Crystal Structure Determination

description: Related Article: Yingying Xu, Wugai An, Wenchao Ding, Haijian Liu, Laijin Tian|2013|Commun.Inorg.Synth.|1|60|
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: 10.5517/ccdc.csd.cc11gmgl
title: CCDC 967369: Experimental Crystal Structure Determination

description: Related Article: Si Yue Wei, Feng Ying Bai, Ge Song, Ya Nan Hou, Xue Ting Xu, Xiao Xi Zhang, Huan Zhi Zhang, Yong Heng Xing|2014|Commun.Inorg.Synth.|2|5|
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: 10.5517/ccdc.csd.cc11gmhm
title: CCDC 967370: Experimental Crystal Structure Determination

description: Related Article: Si Yue Wei, Feng Ying Bai, Ge Song, Ya Nan Hou, Xue Ting Xu, Xiao Xi Zhang, Huan Zhi Zhang, Yong Heng Xing|2014|Commun.Inorg.Synth.|2|5|
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: 10.5281/zenodo.1136213
title: Pyramid Finite Elements For Discontinuous And Continuous Discretizations Of The Neutron Diffusion Equation With Applications To Reactor Physics

description: Data statement for named paper
DOI: 10.5517/ccdc.csd.cc12tkjz
title: CCDC 1007671: Experimental Crystal Structure Determination

description: Related Article: Felicite Majoumo-Mbe, Emmanuel N. Nfor, Eric B. Sengeh, Romanus N. Njong and Offiong E. Offiong|2015|Commun.Inorg.Synth.|3|40|
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: 10.17632/3ft6k9pb9p.1
title: Data for: Fine structure of Leptomyxa ambigua n.sp. CCAP 1546/2 strain, formerly known as “Rhizamoeba flabellata” (Amoebozoa, Tubulinea, Leptomyxida)

description: A videorecord of CCAP 1546/2 strain made in 1999 in CCAp. Windermere by Alexey Smirnov (author)
DOI: 10.5281/zenodo.1136212
title: Pyramid Finite Elements For Discontinuous And Continuous Discretizations Of The Neutron Diffusion Equation With Applications To Reactor Physics

description: Data statement for named paper
DOI: 10.5281/zenodo.1136214
title: Dataset And Supplementary Files_Ict

description: Dataset and supplementary files of the study: Development of a scale to know the basic skills in the use of ICT in educative settings, that could be applied to students and teachers alike in the secondary and high school levels.
DOI: 10.5517/ccdc.csd.cc1n6yyr
title: CCDC 1526035: Experimental Crystal Structure Determination

description: Related Article: Nicole Dinamarca, Pedro Levín, Hugo Muñoz, Francesco Caruso, Miriam Rossi, Juan Guerrero and Manuel Ignacio Azócar|2017|Commun.Inorg.Synth.|5|11|
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: 10.5517/ccdc.csd.cc1pdf6q
title: CCDC 1561073: Experimental Crystal Structure Determination

description: Related Article: Johannes Prock, Simon Salzl, Katharina Ehrmann, Wolfgang Viertl, Richard Pehn, Johann Pann, Helena Roithmeyer, Marvin Bendig, Holger Kopacka, Laura Capozzoli, Werner Oberhauser, Günther Knör, Peter Brüggeller|2018|ChemPhotoChem|2|271|doi:10.1002/cptc.201700115
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: 10.5517/ccdc.csd.cc1pdf7r
title: CCDC 1561074: Experimental Crystal Structure Determination

description: Related Article: Johannes Prock, Simon Salzl, Katharina Ehrmann, Wolfgang Viertl, Richard Pehn, Johann Pann, Helena Roithmeyer, Marvin Bendig, Holger Kopacka, Laura Capozzoli, Werner Oberhauser, Günther Knör, Peter Brüggeller|2018|ChemPhotoChem|2|271|doi:10.1002/cptc.201700115
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: 10.5517/ccdc.csd.cc1pbx31
title: CCDC 1559613: Experimental Crystal Structure Determination

description: Related Article: Felipe López-Saucedo, G. Gabriel Flores-Rojas, Lucero González-Sebastián, Reyna Reyes-Martínez, Juan Manuel German-Acacio, Alcives Avila-Sorrosa, Simón Hernández-Ortega, David Morales-Morales|2018|Inorg.Chim.Acta|473|83|doi:10.1016/j.ica.2017.12.029
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: 10.5517/ccdc.csd.cc1pbx42
title: CCDC 1559614: Experimental Crystal Structure Determination

description: Related Article: Felipe López-Saucedo, G. Gabriel Flores-Rojas, Lucero González-Sebastián, Reyna Reyes-Martínez, Juan Manuel German-Acacio, Alcives Avila-Sorrosa, Simón Hernández-Ortega, David Morales-Morales|2018|Inorg.Chim.Acta|473|83|doi:10.1016/j.ica.2017.12.029
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.5005490
title: Early Cretaceous magmatism and associated polymetallic mineralization in South China: the Tiantang example

description: The Tiantang Cu–Pb–Zn polymetallic deposit in western Guangdong, South China, is hosted in the contact zone between the monzogranite porphyry and limestone of the Devonian Tianziling Formation. Orebodies occur in the skarn and skarnized marble as bedded, lenses, and irregular shapes. In this study, we performed LA-ICP-MS zircon U–Pb dating, zircon trace elements, and Hf isotopic analyses on the Tiantang monzogranite porphyry closely related to Cu–Pb–Zn mineralization. Twenty-two zircons from the sample yield excellent concordia results with a weighted mean <sup>206</sup>Pb/<sup>238</sup>U age of 104.5 ± 0.7 Ma, which shows that the emplacement of the monzogranite porphyry in the Tiantang deposit occurred in the Early Cretaceous. The zircon U–Pb age is largely consistent with the sulphide Rb–Sr isochron ages, indicating that both the intrusion and Cu–Pb–Zn mineralization were formed during the Early Cretaceous in South China. The <i>ε</i><sub>Hf</sub>(<i>t</i>) values of three inherited zircons from the monzogranite porphyry are 13.1, 11.9, and 12.9, respectively, and the two-stage Hf model ages are 1096 Ma, 1087 Ma, and 1055 Ma, respectively. Except for the three inherited zircons, all <i>ε</i><sub>Hf</sub>(<i>t</i>) values of zircons are negative and have a range of −7.6 to −3.4, with the two-stage model ages (T<sub>DM2</sub>) of 1380–1643 Ma, which indicates the rock-forming materials were mainly derived from the partial melting of Mesoproterozoic to Neoproterozoic crust rocks, and probably included some Neoproterozoic arc-related volcanic-sedimentary materials. In this study, the monzogranite porphyry from the Tiantang deposit has calculated Ce<sup>4+</sup>/Ce<sup>3+</sup> ratios of zircon ranging from 91 to 359, indicative of a more oxidized signature and significant prospecting potential for ore-related magmatism. Based on ore deposit geology, isotope geochemistry, and geochronology of the Tiantang Cu–Pb–Zn deposit and regional geodynamic evolution, the formation of Early Cretaceous magmatism and associated polymetallic mineralization in South China is believed to be related to large-scale continental extension and subsequent upwelling of the asthenosphere.
DOI: 10.6084/m9.figshare.5005490.v1
title: Early Cretaceous magmatism and associated polymetallic mineralization in South China: the Tiantang example

description: The Tiantang Cu–Pb–Zn polymetallic deposit in western Guangdong, South China, is hosted in the contact zone between the monzogranite porphyry and limestone of the Devonian Tianziling Formation. Orebodies occur in the skarn and skarnized marble as bedded, lenses, and irregular shapes. In this study, we performed LA-ICP-MS zircon U–Pb dating, zircon trace elements, and Hf isotopic analyses on the Tiantang monzogranite porphyry closely related to Cu–Pb–Zn mineralization. Twenty-two zircons from the sample yield excellent concordia results with a weighted mean <sup>206</sup>Pb/<sup>238</sup>U age of 104.5 ± 0.7 Ma, which shows that the emplacement of the monzogranite porphyry in the Tiantang deposit occurred in the Early Cretaceous. The zircon U–Pb age is largely consistent with the sulphide Rb–Sr isochron ages, indicating that both the intrusion and Cu–Pb–Zn mineralization were formed during the Early Cretaceous in South China. The <i>ε</i><sub>Hf</sub>(<i>t</i>) values of three inherited zircons from the monzogranite porphyry are 13.1, 11.9, and 12.9, respectively, and the two-stage Hf model ages are 1096 Ma, 1087 Ma, and 1055 Ma, respectively. Except for the three inherited zircons, all <i>ε</i><sub>Hf</sub>(<i>t</i>) values of zircons are negative and have a range of −7.6 to −3.4, with the two-stage model ages (T<sub>DM2</sub>) of 1380–1643 Ma, which indicates the rock-forming materials were mainly derived from the partial melting of Mesoproterozoic to Neoproterozoic crust rocks, and probably included some Neoproterozoic arc-related volcanic-sedimentary materials. In this study, the monzogranite porphyry from the Tiantang deposit has calculated Ce<sup>4+</sup>/Ce<sup>3+</sup> ratios of zircon ranging from 91 to 359, indicative of a more oxidized signature and significant prospecting potential for ore-related magmatism. Based on ore deposit geology, isotope geochemistry, and geochronology of the Tiantang Cu–Pb–Zn deposit and regional geodynamic evolution, the formation of Early Cretaceous magmatism and associated polymetallic mineralization in South China is believed to be related to large-scale continental extension and subsequent upwelling of the asthenosphere.
DOI: 10.6084/m9.figshare.7102373
title: Penetration performance of axisymmetric U-shape-nose grooved projectile into aluminum target: Theoretical model and experiment

description: Abstract The penetration performance of projectiles is closely related to their nose shape as it influences the kinetic energy penetration of a rigid projectile. One new type of projectile, which is entitled U-shape-nose grooved projectile, is introduced in this study. A theoretical model, which describes the structural characterization of U-shape-nose grooved projectile, is constructed here to investigate the penetration characters into an aluminum target. Moreover, comparative penetration experiments were conducted to investigate the penetration performance of U-shape-nose grooved projectile. Effects of characteristic parameters and shape optimal conditions of the U-shape-nose grooved projectile on the penetration performance are analyzed with the theoretical model validated by the experimental results. It has been proved that U-shape-nose grooved projectile has a more excellent penetration performance than the ogive-nose projectile based on comparison between the results of experimental and theoretical model. The projectile with U-shape-nose grooves sharpens the nose of the projectile and changes the failure mode of target during penetration, which has advantages of decreasing penetration resistance and enhancing the depth of penetration.
DOI: 10.6084/m9.figshare.16539559.v1
title: Miocene adakitic volcanism in eastern Lhasa Terrane, Tibet: perspective from zircon U–Pb geochronology, whole-rock geochemistry and Sr–Nd–Hf isotopes

description: The Riduo intermediate-felsic volcanic rocks are located in the eastern Lhasa terrane in southern Tibet. Zircon U–Pb dating, geochemical and Sr–Nd–Hf isotope analyses were carried out to constrain the age, petrogenesis and magma source of the Riduo magma suite, including andesite, dacitic tuff, and quartz diorite. Zircon U–Pb dating yielded Early Miocene ages of 19.5 ± 0.5 Ma (andesite), 17.6 ± 0.3 Ma (dacitic tuff), and 15.6 ± 0.5 Ma (quartz diorite). Geochemically, this early Miocene suite is adakitic with high SiO<sub>2</sub> (55.76–69.46 wt.%), Al<sub>2</sub>O<sub>3</sub> (15.21–16.61 wt.%), Na<sub>2</sub>O (3.82–4.83 wt.%), Sr (427–1033 ppm), and Sr/Y (24.5–145), but low Y (&lt; 17.8 ppm) and Yb (&lt; 1.82 ppm). The rocks also have low to high K<sub>2</sub>O (0.44–3.82 wt.%). They are enriched in light rare earth elements (LREEs), large ion lithophile elements (LILEs, e.g. K, Rb, Th and U), but depleted in high-field strength elements (e.g. Nb, Ta) and heavy rare earth elements (HREEs), and have weakly negative to positive Eu anomalies. Isotope analyses reveal that most samples have high whole-rock initial <sup>87</sup>Sr/<sup>86</sup>Sr ratios (0.705611–0.708807), low ε<sub>Nd</sub>(t) (−2.25 to −1.15), and positive zircon ε<sub>Hf</sub> (t) (+1.29 to +6.49). We suggest that the early Miocene magmas in the eastern Lhasa terrane were likely sourced from post-collisional partial melting of the juvenile lower crust with minor mantle input. The magmas may have been crustal-contaminated during their ascent to the upper crust along the N-S-trending Cona-Riduo rift.
DOI: 10.6084/m9.figshare.12344948
title: Additional file 2 of Rno-microRNA-30c-5p promotes myocardial ischemia reperfusion injury in rats through activating NF-κB pathway and targeting SIRT1

description: Additional File 2. Table S2. Predicted details of SIRT1R4
DOI: 10.6084/m9.figshare.11821317.v1
title: Geochronology and petrogenesis of the Late Silurian Shitoukengde mafic–ultramafic intrusion, NW China: Implications for the tectonic setting and magmatic Ni-Cu mineralization in the East Kunlun Orogenic Belt

description: The Shitoukengde mafic–ultramafic intrusion, located in the East Kunlun Orogenic Belt, is spatially and temporally associated with the Xiarihamu Ni-Cu sulphide deposit, the second-largest Ni deposit in China. This intrusion comprises mainly lherzolite, harzburgite, olivine websterite, and gabbroic rocks. The Shitoukengde mafic–ultramafic rocks are enriched in light rare earth elements (REE) relative to heavy REE and show pronounced negative Nb–Ta anomalies. Magmatic zircon crystals of the studied samples have high δ<sup>18</sup>O values (6.5 to 8.0‰) with a weighted mean value of 7.3‰ that is higher than the typical mantle value (~5.3‰). They are characterized by high ε<sub>Hf</sub>(t) values (–2.0 to 9.2) and variable ε<sub>Nd</sub>(t) values (–4.46 to 2.83). Olivine grains from the ultramafic rocks have high forsterite (Fo) values of 79.3–86.8 and variable Ni contents of 746–3347 ppm. Our calculations indicate that parental magma of the Shitoukengde intrusion had a high-Mg basaltic composition with 10.9 wt% MgO and 9.8 wt% FeO<sup>T</sup>. Fractional crystallization and significant crustal contamination triggered S saturation and sulphide enrichment in the magma. Zircon LA-ICPMS and SIMS U–Pb analyses reveal the consistent Silurian ages of 420–424 Ma for the gabbronorite and Ol websterite, which is coeval with the Xiarihamu Ni-Cu deposit. Based on these data and the regional tectonic setting, we suggest that the Shitoukengde mafic-ultramafic rocks formed in the post-collisional, extensional environment. The cessation of subduction may have resulted in break-off of the dense subducted slab, and triggered ascent of the hot convective asthenospheric mantle. The mantle wedge was modified by the subduction-related fluids and these enriched mantle components were incorporated into the ascending asthenospheric melts at relatively shallow depths, generating the high-Mg basaltic magmas that formed the compositionally variable mafic-ultramafic rocks (e.g., Shitoukengde and Xiarihamu intrusions) in the Eastern Kunlun Orogenic belt.
DOI: 10.6084/m9.figshare.21256918
title: Additional file 6 of Identification of SSBP1 as a ferroptosis-related biomarker of glioblastoma based on a novel mitochondria-related gene risk model and in vitro experiments

description: Additional file 6: Table S1. The mitochondria-related genes extracted from the uniprot database.
DOI: 10.6084/m9.figshare.11821443
title: Crystal structure and anti-breast cancer activity evaluation of a nanosized bismuth(V)-containing coordination complex based on the F-decorated ligand

description: In the current study, a new heteroleptic triorganobismuth (V) complex with the chemical formula of Bi(phenyl)<sub>3</sub>(2,3-dfa)<sub>2</sub> has been successfully prepared by using C donor phenyl ring and O donor 2,3-difluorobenzoic acid (2,3-H<sub>2</sub>dfa) ligands, which has been fully characterized by single crystal X‐ray crystallography, elemental analysis, powder X-ray diffraction along with the thermogravimetric analysis. Furthermore, a green hand grinding technique was used to get the nanocrystals of <b>1</b> with an average size of 200 nm as revealed via the scanning electron microscopy (SEM). The inhibitory effect of BT474 cells proliferation after nano <b>1</b> treatment was detected with CCK-8 assay. The apoptosis of BT474 cells was measured with FITC-Annexin V/PI double staining assay, the influence on ROS accumulation was determined with DCFH-DA staining.
DOI: 10.6084/m9.figshare.16539656
title: Spatial-temporal distribution and tectonic setting of Mesozoic W-mineralized granitoids in the Xing-Meng Orogenic Belt, NE China

description: The Xing-Meng Orogenic Belt is characterized by intense and widespread Mesozoic granitic magmatism related to large-scale W mineralization. Three periods of W-mineralized granitic magmatism can be distinguished: Early Triassic, Early–Middle Jurassic, and Late Jurassic–Early Cretaceous. Early Mesozoic W-mineralized granitoids are I-type granites with metaluminous to weakly peraluminous characteristics, with higher Rb concentrations and lower K/Rb ratios than coeval W-barren granitoids. Late Mesozoic W-mineralized granitoids belong to highly fractionated A-type granites, enriched in Rb, Th, and U, and depleted in Ba, Sr, P, Ti, and Eu. They have higher Rb/Sr and U/Th ratios, and lower (La/Yb)<sub>N</sub>, LREE/HREE, Eu/Eu*, K/Rb, Zr/Hf, Nb/Ta, and Y/Ho ratios than contemporary W-barren granitoids. Mesozoic W-mineralized granitoids mainly originated from the partial melting of juvenile lower crust, whereas Early Mesozoic W-mineralized granitoids encompassed minor reworked ancient crustal material. Triassic W-mineralized granitoids formed in a syn- and/or post-collision setting related to the closure of Paleo-Asian Ocean. Early–Middle Jurassic W-mineralized granitoids formed in a compressional setting created by the subduction of Paleo-Pacific Ocean plate in the east and the closure of Mongol-Okhotsk Ocean in the west. Late Mesozoic W-mineralized granitoids formed in a post-orogenic extensional setting controlled by the MOO and PPO tectonic regimes.
DOI: 10.6084/m9.figshare.16539656.v1
title: Spatial-temporal distribution and tectonic setting of Mesozoic W-mineralized granitoids in the Xing-Meng Orogenic Belt, NE China

description: The Xing-Meng Orogenic Belt is characterized by intense and widespread Mesozoic granitic magmatism related to large-scale W mineralization. Three periods of W-mineralized granitic magmatism can be distinguished: Early Triassic, Early–Middle Jurassic, and Late Jurassic–Early Cretaceous. Early Mesozoic W-mineralized granitoids are I-type granites with metaluminous to weakly peraluminous characteristics, with higher Rb concentrations and lower K/Rb ratios than coeval W-barren granitoids. Late Mesozoic W-mineralized granitoids belong to highly fractionated A-type granites, enriched in Rb, Th, and U, and depleted in Ba, Sr, P, Ti, and Eu. They have higher Rb/Sr and U/Th ratios, and lower (La/Yb)<sub>N</sub>, LREE/HREE, Eu/Eu*, K/Rb, Zr/Hf, Nb/Ta, and Y/Ho ratios than contemporary W-barren granitoids. Mesozoic W-mineralized granitoids mainly originated from the partial melting of juvenile lower crust, whereas Early Mesozoic W-mineralized granitoids encompassed minor reworked ancient crustal material. Triassic W-mineralized granitoids formed in a syn- and/or post-collision setting related to the closure of Paleo-Asian Ocean. Early–Middle Jurassic W-mineralized granitoids formed in a compressional setting created by the subduction of Paleo-Pacific Ocean plate in the east and the closure of Mongol-Okhotsk Ocean in the west. Late Mesozoic W-mineralized granitoids formed in a post-orogenic extensional setting controlled by the MOO and PPO tectonic regimes.
DOI: 10.6084/m9.figshare.21256947.v1
title: Additional file 1 of Sequencing individual genomes with recurrent genomic disorder deletions: an approach to characterize genes for autosomal recessive rare disease traits

description: Additional file 1: Table S1. All clinically reported recurrent deletions and their prevalence estimates. Table S2. All 717 recurrent genomic deletions predicted based on the repeat structure in the human reference genome GRCh38. Table S3. Carrier disease allele frequencies by allele. Table S4. Carrier allele frequency burden by gene. The list is ranked by genes from the highest burden to the lowest burden. The frequency burden in this list only includes the actual observed variants; the 10% extra hypothetical uncharacterized alleles as described in the Methods section are not included. Table S5. Gene-level NAHR contribution to carrier allele and recessive disease burden as well as NAHR Deletion Impact to Recessive Traits (DIRT). This table is comprised of five panels, representing results generated using data from the general population and four specific ethnic groups, including African (AFR), Latino (AMR), East Asian (EAS), and European (EUR). Table S6. Meta-analyses for literature reported patients affected with the 13 recessive disorders contributed by significant NAHR-mediated deletion burden. Compound heterozygous variants are split into two rows with each row representing one variant. Table S7. Molecular findings of recurrent deletions identified from clinical exome sequencing. Table S8. Literature review for 15q13.3 recurrent deletions.