cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.5281/zenodo.8106250
title: Mutation Effect Prediction of Proteins using RoseTTAFold

description: Deep mutational scanning datasets used for 'Mutation Effect Prediction of Proteins using RoseTTAFold'. Target MSAs, RF predicted PDBs and experimental values (csvs) are provided. Results published and referenced in paper are also provided.
DOI: 10.5281/zenodo.7662433
title: Mutation Effect Prediction of Proteins using RoseTTAFold

description: Deep mutational scanning datasets used for 'Mutation Effect Prediction of Proteins using RoseTTAFold'. Target MSAs, RF predicted PDBs and experimental values (csvs) are provided. Results published and referenced in paper are also provided.
DOI: 10.34740/kaggle/dsv/6206933
title: Youtube Trending Video - Taiwan & Hong Kong
DOI: 10.13140/rg.2.2.17241.08805
title: Programa con algoritmo de inteligencia artificial de filtro AMARILLO/ROJO/AZUL para edición de fotografías en lenguaje Python
DOI: 10.13140/rg.2.2.30662.86087
title: Programa con algoritmo de inteligencia artificial de filtro AMARILLO/ROJO/AZUL para edición de fotografías en lenguaje Python
DOI: 10.13140/rg.2.2.13885.64489
title: Programa con algoritmo de inteligencia artificial de filtro AMARILLO/ROJO/AZUL para edición de fotografías en lenguaje Python
DOI: 10.6084/m9.figshare.23207096
title: Geochemical characteristics and structural setting of lithium–caesium–tantalum pegmatites of the Dorchap Dyke Swarm, northeast Victoria, Australia

description: The Dorchap Dyke Swarm hosts the first recorded occurrence of lithium–caesium–tantalum (LCT) pegmatites in Victoria, Australia. Syn-orogenic emplacement of pegmatite dykes occurred along a northwest-trending shear system during the Benambran Orogeny. Pegmatites are derived from fractionated melt associated with the Mount Wills Granite, which is an S-type, peraluminous granite originating from supracrustal melting of Ordovician sedimentary sequences. A distinct, eastward-oriented fractionation trend across the Dorchap Dyke Swarm has highlighted a 20 × 8 km highly fractionated zone in the northeastern Dorchap Range, which includes spodumene- and petalite-bearing pegmatites. A distinct pattern of elemental enrichment (P &gt; Cs &gt; Be &gt; Nb ≥ Ta &gt; Li &gt; Sn) is observed across the strongly fractionated zone of the Dorchap Dyke Swarm. Subsequent metasomatic fluid movements and hydrothermal overprinting have resulted in redistribution of mobile elements in the Dorchap Range, either as hydrothermal alteration species or in some instances as the development of exomorphic halos. Additionally, a regional alteration overprint, likely associated with subsequent metamorphism of pegmatite dykes has resulted in alteration of primary petalite to spodumene plus quartz, and primary spodumene to cookeite. Bulk rock geochemical data from the Dorchap Dyke Swarm suggest a syn-collisional setting for dyke intrusion, consistent with the inferred tectonic setting of the central Lachlan Fold Belt at the time of pegmatite emplacement. Pegmatite dykes locally contain an overprinted structural foliation, which is consistent with the primary structural trend of deformed metasediments and may indicate that dyke emplacement was syngenetic with regional folding and compression of the surrounding Omeo Metamorphic Complex during the Benambran Orogeny. Subsequent hydrothermal alteration of some dykes likely occurred immediately following the Bindian Orogeny.KEY POINTSDorchap Dyke Swarm are the first recorded Li–Cs–Ta pegmatites in Victoria, Australia.Pegmatites were emplaced synchronous with or immediately following the Benambran Orogeny.Dorchap Dyke Swarm pegmatites are geochemically correlated with the Mount Wills Granite. Dorchap Dyke Swarm are the first recorded Li–Cs–Ta pegmatites in Victoria, Australia. Pegmatites were emplaced synchronous with or immediately following the Benambran Orogeny. Dorchap Dyke Swarm pegmatites are geochemically correlated with the Mount Wills Granite.
DOI: 10.6084/m9.figshare.23598716
title: Zircon age distributions and implied tectonic settings of early Cambrian to Early Devonian sedimentation in western and central Victoria

description: Age distributions among the detrital zircon populations in western and central Victorian Paleozoic metasedimentary rocks suggest that most were deposited in Andean-type back-arc environments, with variable proportions of arc and continental sediment sources. Notable exceptions are the upper Cambrian Knowsley East Shale and the Silurian(?) sample of ‘Glen Creek Lithic Sandstone’, which both contain unimodal zircon populations. In the case of the Knowsley East Shale, this age is very close to the inferred depositional age, implying a possible forearc environment, with sediment derived directly from the contemporary volcanic arc. On the other hand, the implied trench environment for the ‘Glen Creek Lithic Sandstone’ is most likely inherited from its very local sediment source in the fault-bounded and mainly Cambrian Glen Creek erosional window. The only analysed rock units that may have been deposited in non-arc settings are the middle Silurian Humevale Siltstone and the Lower Devonian Norton Gully Sandstone. The zircon populations in these units carry strong continental signals, and they may have been deposited in an extensional marine basin bounded by continental blocks. The upper Silurian Grampians Group may have been deposited in a similar rift setting, but the zircon age histogram for this unit suggests that it was more proximal to an arc terrane. These assignments of depositional/tectonic environment should be regarded as indicative only, particularly since the method provides only subtle distinctions between some extensional and convergent settings. However, if the assignments are correct, there are some important implications for the geological history of this part of the Lachlan Orogen. For example, contrary to present perceptions, the Stawell Zone rocks may not have been prominently uplifted during the Ordovician, and the basin in the Bendigo Zone may have been receiving sediment input from further west in the Grampians–Stavely Zone. Early Cambrian to Early Devonian sedimentation in western and central Victoria occurred mainly in back-arc marine basins, initially associated with an Andean-type margin. Locally, some Cambrian sediments were formed in trench or forearc environments, with detritus supplied directly from a contemporary volcanic arc. Cambrian to Silurian back-arc sediments were deposited at varying distances from any active or former arc terranes and with varying but always major contributions of continent-derived sediments. Early Devonian sediments in the Melbourne Zone may have been deposited in what was effectively an intracontinental marine rift.
DOI: 10.6084/m9.figshare.23681896
title: The isotope geochemistry of host rocks of the late Archean Guandi and Banshigou banded iron formations, southern Jilin Province: temporal and tectonic significance

description: The Guandi and Banshigou iron deposits of southern Jilin Province, China, are Algoma-type banded iron formations (BIFs) located in the Eastern Block of the North China Craton (NCC). LA–ICP–MS U–Pb dating shows the magmatic zircons in plagioclase amphibolite from the Guandi BIF (PA–GD) and plagioclase hornblende gneiss from the Banshigou BIF (PHG–BSG) were crystallised at 2556 ± 17 Ma and 2545 ± 27 Ma, respectively, representing the formation age of the BIFs. Metamorphic overgrowth zircons from both samples gave two U–Pb ages of 2452 ± 23 Ma and 2446 ± 70 Ma, indicating the age of metamorphism. The zircon ε<sub>Hf</sub>(t) values of PA–GD (–1.3 to +2.8) and PHG–BSG (–1.5 to +2.7) indicate that the magma source was derived from depleted mantle with contamination of crustal material. According to our study, the PA–GD and PHG–BSG were formed in an island arc setting and support previously proposed subduction zone tectonic models for the northeastern NCC during the Neoarchean. The magmatic zircons from the PA–GD and PHG–BSG were crystallised at 2556 ± 17 Ma and 2545 ± 27 Ma, which represents the formation age of the BIFs. The metamorphic overgrowth zircons from the PA–GD and PHG–BSG gave two ages of 2452 ± 23 Ma and 2446 ± 70 Ma, which represent the age of metamorphism. Major-element and REE data indicate that BIFs precipitated in a mixture of seawater and hydrothermal fluids in an anoxic environment. Geochemical and Hf isotope characteristics of BIFs’ wall rock indicate that the source magma was derived from a depleted mantle wedge metasomatised by subduction-slab melts and contaminated by ancient crust, formed in an island arc setting.
DOI: 10.6084/m9.figshare.23598716.v1
title: Zircon age distributions and implied tectonic settings of early Cambrian to Early Devonian sedimentation in western and central Victoria

description: Age distributions among the detrital zircon populations in western and central Victorian Paleozoic metasedimentary rocks suggest that most were deposited in Andean-type back-arc environments, with variable proportions of arc and continental sediment sources. Notable exceptions are the upper Cambrian Knowsley East Shale and the Silurian(?) sample of ‘Glen Creek Lithic Sandstone’, which both contain unimodal zircon populations. In the case of the Knowsley East Shale, this age is very close to the inferred depositional age, implying a possible forearc environment, with sediment derived directly from the contemporary volcanic arc. On the other hand, the implied trench environment for the ‘Glen Creek Lithic Sandstone’ is most likely inherited from its very local sediment source in the fault-bounded and mainly Cambrian Glen Creek erosional window. The only analysed rock units that may have been deposited in non-arc settings are the middle Silurian Humevale Siltstone and the Lower Devonian Norton Gully Sandstone. The zircon populations in these units carry strong continental signals, and they may have been deposited in an extensional marine basin bounded by continental blocks. The upper Silurian Grampians Group may have been deposited in a similar rift setting, but the zircon age histogram for this unit suggests that it was more proximal to an arc terrane. These assignments of depositional/tectonic environment should be regarded as indicative only, particularly since the method provides only subtle distinctions between some extensional and convergent settings. However, if the assignments are correct, there are some important implications for the geological history of this part of the Lachlan Orogen. For example, contrary to present perceptions, the Stawell Zone rocks may not have been prominently uplifted during the Ordovician, and the basin in the Bendigo Zone may have been receiving sediment input from further west in the Grampians–Stavely Zone. Early Cambrian to Early Devonian sedimentation in western and central Victoria occurred mainly in back-arc marine basins, initially associated with an Andean-type margin. Locally, some Cambrian sediments were formed in trench or forearc environments, with detritus supplied directly from a contemporary volcanic arc. Cambrian to Silurian back-arc sediments were deposited at varying distances from any active or former arc terranes and with varying but always major contributions of continent-derived sediments. Early Devonian sediments in the Melbourne Zone may have been deposited in what was effectively an intracontinental marine rift.
DOI: 10.13140/rg.2.2.27307.41769
title: The Pro-Ukraine and pro-Zelensky double theorem
DOI: 10.13140/rg.2.2.20596.53123
title: The Pro-Ukraine and pro-Zelensky double theorem
DOI: 10.13140/rg.2.2.34018.30403
title: The Pro-Ukraine and pro-Zelensky double theorem
DOI: 10.13140/rg.2.2.13046.78403
title: The Pro-Ukraine and pro-Zelensky double theorem(Revised and Coded)
DOI: 10.25442/hku.23701179
title: Supporting data for "A (Bio)chemo-hydro-mechanical Framework for Enhanced Cracking in Geomaterials"

description: This is the supporting data for "A (Bio)chemo-hydro-mechanical Framework for Enhanced Cracking in Geomaterials". The file name includes the chapter number corresponding to the chapter list in the PhD thesis.
DOI: 10.25442/hku.23706837
title: <strong>Supporting data for "Random forest boosts genetic risk prediction of systemic lupus erythematosus (SLE) but does not distinguish between patients with lupus nephritis (LN) and non-LN"</strong>

description: Systemic lupus erythematosus (SLE) is a classic autoimmune disease that affects several vital organs throughout the body, including the heart, brain, kidneys, joints, skin and central nervous system. Conventional method of Polygenetic Risk Score (PRS) does not consider the relationships between alleles. Hence, we proposed to apply three classical supervised ML models, Random Forest (RF), Support Vector Machine (SVM) and Artificial Neural Network (ANN), whose typical characteristic is to capture correlations of genetic features, to improve the predictions for risks of developing SLE.
DOI: 10.25442/hku.23706837.v1
title: <strong>Supporting data for "Random forest boosts genetic risk prediction of systemic lupus erythematosus (SLE) but does not distinguish between patients with lupus nephritis (LN) and non-LN"</strong>

description: Systemic lupus erythematosus (SLE) is a classic autoimmune disease that affects several vital organs throughout the body, including the heart, brain, kidneys, joints, skin and central nervous system. Conventional method of Polygenetic Risk Score (PRS) does not consider the relationships between alleles. Hence, we proposed to apply three classical supervised ML models, Random Forest (RF), Support Vector Machine (SVM) and Artificial Neural Network (ANN), whose typical characteristic is to capture correlations of genetic features, to improve the predictions for risks of developing SLE.
DOI: 10.15468/dl.4vrpay
title: Occurrence Download

description: A dataset containing 0 species occurrences available in GBIF matching the query: { "TaxonKey" : [ "is Diplacrum poklei (Wad.Khan) K.C.Mohan" ] } The dataset includes 0 records from 0 constituent datasets:
DOI: 10.6084/m9.figshare.23796657
title: Table 5: The results of the analysis of the topic of the article

description: This table contains information about the results of the analysis of the topic of the article
DOI: 10.6084/m9.figshare.23796657.v1
title: Table 5: The results of the analysis of the topic of the article

description: This table contains information about the results of the analysis of the topic of the article
DOI: 10.6084/m9.figshare.23796624
title: The genome assembly and annotation of Y476

description: Assembly and annotation of the Haplotype genome of Y476<br>
DOI: 10.25442/hku.23701179.v1
title: Supporting data for "A (Bio)chemo-hydro-mechanical Framework for Enhanced Cracking in Geomaterials"

description: This is the supporting data for "A (Bio)chemo-hydro-mechanical Framework for Enhanced Cracking in Geomaterials". It includes numerical input files and mesh files for three case studies which are (1) Reactive-Chemo-Mechanical Model for Weak Acid-Assisted Cavity Expansion in Carbonate Rocks, (2) Acid-Assisted Subcritical Blunt-tip Crack Propagation in Carbonate Rocks, (3) Reactive Chemo-Hydro-Mechanics for Cavity Expansion in A Dissolvable Geomaterial. All of the studies are associated with the fundamental problem of elasto-plastic expansion around a cylindrical cavity/crack under the combined effect of fluid pressurization and chemical softening due to the geomaterial’s susceptibility to mineral mass dissolution in the presence of acidity. The file name includes the chapter number corresponding to the chapter list in the PhD thesis.
DOI: 10.5281/zenodo.8190022
title: CREST_input

description: It is the inputs of CREST MODEL, sharing which for publication.
DOI: 10.5281/zenodo.6450539
title: Data from: Holocene Sediment Provenance Evolution in the Northern South China Sea Inferred from Detrital Zircon Geochronology

description: The supporting information here provides the AMS <sup>14</sup>C geochronological data of core sediments (Table S1) and LA-ICP-SF-MS U-Pb results of detrital zircon grains (Table S2) within this study.
DOI: 10.5281/zenodo.8190021
title: CREST_input

description: It is the inputs of CREST MODEL, sharing which for publication.
DOI: 10.5281/zenodo.6450538
title: Data from: Holocene Sediment Provenance Evolution in the Northern South China Sea Inferred from Detrital Zircon Geochronology

description: The supporting information here provides the AMS <sup>14</sup>C geochronological data of core sediments (Table S1) and LA-ICP-SF-MS U-Pb results of detrital zircon grains (Table S2) within this study.
DOI: 10.15468/dl.zrp42t
title: Occurrence Download

description: A dataset containing 0 species occurrences available in GBIF matching the query: { "TaxonKey" : [ "is Scleria swamyi Govind." ] } The dataset includes 0 records from 0 constituent datasets:
DOI: 10.5517/ccdc.csd.cc2dkbq1
title: CCDC 2221203: Experimental Crystal Structure Determination

description: Related Article: Steven K. Butler, Ethan P. Ashbrook, Ian A. Tonks|2023|Organometallics|42|1732|doi:10.1021/acs.organomet.2c00593
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.cc2dkbr2
title: CCDC 2221204: Experimental Crystal Structure Determination

description: Related Article: Steven K. Butler, Ethan P. Ashbrook, Ian A. Tonks|2023|Organometallics|42|1732|doi:10.1021/acs.organomet.2c00593
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.cc2dkbs3
title: CCDC 2221205: Experimental Crystal Structure Determination

description: Related Article: Steven K. Butler, Ethan P. Ashbrook, Ian A. Tonks|2023|Organometallics|42|1732|doi:10.1021/acs.organomet.2c00593
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.cc2dkbt4
title: CCDC 2221206: Experimental Crystal Structure Determination

description: Related Article: Steven K. Butler, Ethan P. Ashbrook, Ian A. Tonks|2023|Organometallics|42|1732|doi:10.1021/acs.organomet.2c00593
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.cc2dxh1w
title: CCDC 2231908: Experimental Crystal Structure Determination

description: Related Article: Niklas Klangwart, Céline Ruijs, Chris S. Hawes, Thorfinnur Gunnlaugsson, Oxana Kotova|2023|Supramol.Chem.|34|10|doi:10.1080/10610278.2023.2177162
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: 10.25912/rdf_1690510751649
title: Reproducibility of the computational fluid dynamic analysis of a cerebral aneurysm monitored over a decade
DOI: 10.5439/1992435
title: tsimovie (a1)

description: The total sky imager (TSI) measures the fraction of the sky view covered by clouds. It provides time series of hemispheric sky images during daylight hours and retrievals of fractional sky cover for periods when the solar elevation is greater than 10 degrees. To view current sky cover retrievals at the ARM sites, see the TSI most recent sky images.
DOI: 10.5439/1992437
title: iapavg (a1)

description: The In Situ Aerosol Profiles (IAP) campaign is a joint effort between the Atmospheric Radiation Measurement (ARM) user facility and the Climate Monitoring and Diagnostics Laboratory (CMDL) of the U.S. National Oceanic and Atmospheric Administration (NOAA). The objective is to obtain a statistically significant data set of the vertical distribution of aerosol properties (e.g., light scattering and absorption, particle chemistry) by flying a Cessna light aircraft over the SGP site. By using a similar aerosol instrument package as the aerosol observing system (AOS) at SGP, the aircraft will fly level legs at altitudes between 500 m and 3500 m several times per week. See the IAP website for more information.
DOI: 10.5439/1992438
title: iap (a1)

description: The In Situ Aerosol Profiles (IAP) campaign is a joint effort between the Atmospheric Radiation Measurement (ARM) user facility and the Climate Monitoring and Diagnostics Laboratory (CMDL) of the U.S. National Oceanic and Atmospheric Administration (NOAA). The objective is to obtain a statistically significant data set of the vertical distribution of aerosol properties (e.g., light scattering and absorption, particle chemistry) by flying a Cessna light aircraft over the SGP site. By using a similar aerosol instrument package as the aerosol observing system (AOS) at SGP, the aircraft will fly level legs at altitudes between 500 m and 3500 m several times per week. See the IAP website for more information.
DOI: 10.5439/1992443
title: 180varanal3dcfsr (c1)

description: 180varanal3dcfsr
DOI: 10.25584/1992452
title: SERDP PFAS 2.0 - An infrared spectral database for gas-phase quantitation of volatile per- and polyfluoroalkyl substances (PFAS)

description: We report the construction of a database of vetted infrared spectra specifically targeting volatile fluorocarbon gases that may be emitted during thermal treatment of per- and polyfluoroalkyl substances (PFAS) to assist understanding of treatment processes and improve quantification. To populate this database, protocols derived from the Pacific Northwest National Laboratory (PNNL) infrared spectral database are used, curtailing the species selection for this data set. Each spectrum in the database is a weighted average derived from 10 or more individual measurements at different partial pressures (static method) or flow rates (dissemination method) to yield good fidelity of both strong and weak infrared signatures, with each composite spectrum ranging from = 6500 cm-1 to = 600 cm-1 with an apodized resolution of 0.112 cm-1. This resolution was chosen to fully resolve all spectral features, recognizing that atmospheric pressure broadening results in nearly all ro-vibrational lines having linewidths = 0.1 cm-1. As an example case, application of the database is demonstrated via identification and quantification of dominant 1H-perfluoroheptane and perfluorohept-1-ene fluorocarbon products resulting from thermal decomposition of perfluorooctanoate (PFOA) below 450 °C.
DOI: 10.6084/m9.figshare.23735211
title: Qualitative feedback (comments and suggestions).docx

description: This data shows the qualitative feedback from participants (comments and suggestions), regarding the prototype of the card game "No Gut No Glory".
DOI: 10.6084/m9.figshare.23735211.v2
title: Qualitative feedback (comments and suggestions).docx

description: This data shows the qualitative feedback from participants (comments and suggestions), regarding the prototype of the card game "No Gut No Glory".