cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.5066/f7wq02rm
title: Magnetotelluric sounding data, stations 1 to 12, East-Central Tooele County, Utah, 2003

description: This dataset includes the magnetotelluric (MT) sounding data collected in 2003 along a north-south profile west of Tooele, Utah. It is important to know whether major mining districts in the Northern Nevada Gold Province are underlain by rocks of the Archean Wyoming craton, which are known to contain orogenic gold deposits, or by accreted rocks of the Paleoproterozoic Mojave province. It is also important to know the location and orientation of the Archean/Proterozoic suture zone between these provinces as well as major basement structures within these terranes because they may influence subsequent patterns of sedimentation, deformation, magmatism, and hydrothermal activity. This study was funded by the U.S. Geological Survey's Mineral Resources Program in cooperation with the U.S. Bureau of Land Management.
DOI: 10.5066/f7sj1hpt
title: Magnetotelluric sounding data, stations 1 to 22, Southern San Luis Valley, Colorado, 2006

description: This dataset includes the magnetotelluric (MT) sounding data collected in 2006 in the Southern San Luis Valley, Colorado. The U.S. Geological Survey conducted a series of multidisciplinary studies, including MT surveys, in the San Luis Valley to improve understanding of the hydrogeology of the Santa Fe Group and the nature of the sedimentary deposits comprising the principal groundwater aquifers of the Rio Grande rift. The shallow unconfined and the deeper confined Santa Fe Group aquifers in the San Luis Basin are the main sources of municipal water for the region. The population of the San Luis Valley region is growing rapidly and water shortfalls could have serious consequences. Future growth and land management in the region depend on accurate assessment and protection of the region's groundwater resources.
DOI: 10.5066/f7kk98z1
title: Magnetotelluric sounding data, stations 1-9, Taos Plateau Volcanic Field, New Mexico, 2009

description: This dataset includes the magnetotelluric (MT) sounding data collected in 2009 in and near the San Luis Basin, New Mexico. The U.S. Geological Survey conducted a series of multidisciplinary studies, including MT surveys, in the San Luis Basin to improve understanding of the hydrogeology of the Santa Fe Group and the nature of the sedimentary deposits comprising the principal groundwater aquifers of the Rio Grande rift. The shallow unconfined and the deeper confined Santa Fe Group aquifers in the San Luis Basin are the main sources of municipal water for the region. The population of the San Luis Basin region is growing rapidly and water shortfalls could have serious consequences. Future growth and land management in the region depend on accurate assessment and protection of the region's groundwater resources.
DOI: 10.4121/15121137.v1
title: True owls of Brazil, supplementary material A: Additional figures, maps and tables.

description: This is part of the supplementary materials of a study evaluating the current system of Brazilian strict protected areas using true owls (Strigidae) as indicator group. It includes three appendixes containing: (1) graphics related to PCAs, entrograms, species binary maps, niche and background equivalency tests; (2) citations; and (3) tables with the metrics of the models.
DOI: 10.4121/15121137.v2
title: True owls of Brazil, supplementary material A: Additional figures, maps and tables.

description: This is part of the supplementary materials of a study evaluating the current system of Brazilian strict protected areas using true owls (Strigidae) as indicator group. It includes three appendixes containing: (1) graphics related to PCAs, entrograms, species binary maps, niche and background equivalency tests; (2) citations; and (3) tables with the metrics of the models.
DOI: 10.4121/15121137
title: True owls of Brazil, supplementary material A: Additional figures, maps and tables.

description: This is part of the supplementary materials of a study evaluating the current system of Brazilian strict protected areas using true owls (Strigidae) as indicator group. It includes three appendixes containing: (1) graphics related to PCAs, entrograms, species binary maps, niche and background equivalency tests; (2) citations; and (3) tables with the metrics of the models.
DOI: 10.5066/f7kd1x3x
title: Mines, Mineral Occurrences, and Mining Districts in the Carlin Area, Nevada

description: Sediment hosted gold deposits in Nevada were first mined in the 1960s from open pit mines with large tonnage and low grade resources. Since that time, continuing exploration and discovery have identified extraordinary resources, and together these deposits now form the second-largest gold endowment on Earth, surpassed only by the Witwatersrand Gold Fields of South Africa. The data herein are part of a larger U.S. Geological Survey (USGS) project to develop an updated geospatial database of mines, mineral deposits and mineral regions in the United States. The point and polygon layers within this database represent locations of mines, mineral occurrences (which includes deposits and prospects), and mining districts in an approximately 200-square mile area northwest of Carlin, Nevada. Tables contain additional information such as commodity, geology, deposit types, activity status, deposit resources, and mine production. The extent of surface workings, when visible on imagery, is also captured and shows the relative size of mining operations. All data were compiled from publicly available sources published from 1910 - 2017. Where possible, data were compiled from primary source reports rather than from syntheses of past reports. Although the selected area does not include the entire Carlin Trend, the area, which covers nine 7.5-minute quadrangles, does contain a wide range of deposit types described through a variety of public data and information. These data are being compiled by the USGS Mineral Deposit Database project with support from the Bureau of Land Management. Data have been checked to ensure the accuracy. If any errors are detected, please notify the originating office. The U.S. Geological Survey strongly recommends that careful attention be paid to the metadata file associated with these data.
DOI: 10.5066/f7th8jtn
title: Missouri Breaks Project, Montana - Digitized aeromagnetic data

description: From February 12 to March 8, 1981, EG and G Geometrics conducted an aeromagnetic survey in Montana for Anaconda Copper Company. A Piper Navajo aircraft was used to conducted the survey. The survey was flown along north-south flightlines spaced 660 feet at a nominal height of 450 feet above the terrain. Five uniformly spaced east-west tie-lines were also flown. During processing, the International Geomagnetic Reference Field (IGRF) of 1975 was updated to 1981 and removed from the survey observations. The resultant anomalous magnetic field was contoured at a 4.0 gamma interval and plotted to map sheets. In 2016, the map sheets were scanned, registered, and the contours were digitized. The point data released here were extracted from the digitized contour lines and include: latitude, longitude, and magnetic-field value (gamma).
DOI: 10.5066/f7vt1qjw
title: Mount Baker and Mount Adams Airborne Magnetic and Electromagnetic Survey Data, August 2002, Washington, USA

description: Hydrothermally altered rocks, particularly if water saturated, can weaken stratovolcanoes, thereby increasing the potential for catastrophic sector collapses that can lead to far-traveled, destructive debris flows, which are the largest volcanic hazards for Mount Adams and Mount Baker. Evaluating the hazards associated with such alteration is difficult because much of the alteration is obscured by ice and its depth extent is unknown. Intense hydrothermal alteration significantly reduces the resistivity and magnetization of volcanic rock and therefore hydrothermally altered rocks are identified with helicopter electromagnetic and magnetic measurements at Mount Baker and Mount Adams. High resolution magnetic and electromagnetic data were collected using the RESOLVE multi-coil, multi-frequency electromagnetic system supplemented by a high sensitivity cesium magnetometer. The survey took place out of over Mount Adams and Mount Baker, Washington during May of 2002. The survey covers an area centered on Mount Adams and Mount Baker. Data were collected along north-south flight lines with east-west tie lines. A nominal EM sensor flight height of 60 m was maintained, except where safety dictated a higher elevation. A total of 200 kilometers over the 2 survey blocks were flown. Three files are available in this publication and include flight line data for the magnetic survey, flight line data for the gravity gradiometry survey and a report describing the survey parameters, field operations, quality control and data reduction procedures.
DOI: 10.5517/ccdc.csd.cc296hqr
title: CCDC 2121414: Experimental Crystal Structure Determination

description: Related Article: Amelia M. Swarbrook, Rohan J. Weekes, Jack W. Goodwin, Chris S. Hawes|2022|Dalton Trans.|51|1056|doi:10.1039/D1DT04007C
DOI: 10.5517/ccdc.csd.cc297m8g
title: CCDC 2122485: Experimental Crystal Structure Determination

description: Related Article: W. Kice Brown, Kevin K. Klausmeyer, Brian M. Lindley|2022|Chem.Commun.|58|867|doi:10.1039/D1CC06458D
DOI: 10.5517/ccdc.csd.cc297m9h
title: CCDC 2122486: Experimental Crystal Structure Determination

description: Related Article: W. Kice Brown, Kevin K. Klausmeyer, Brian M. Lindley|2022|Chem.Commun.|58|867|doi:10.1039/D1CC06458D
DOI: 10.5517/ccdc.csd.cc297mbj
title: CCDC 2122487: Experimental Crystal Structure Determination

description: Related Article: W. Kice Brown, Kevin K. Klausmeyer, Brian M. Lindley|2022|Chem.Commun.|58|867|doi:10.1039/D1CC06458D
DOI: 10.5517/ccdc.csd.cc287fjh
title: CCDC 2092516: Experimental Crystal Structure Determination

description: Related Article: Xiaomin Hou, Si-Fu Tang|2022|Dalton Trans.|51|1041|doi:10.1039/D1DT03596G
DOI: 10.5517/ccdc.csd.cc287fkj
title: CCDC 2092517: Experimental Crystal Structure Determination

description: Related Article: Xiaomin Hou, Si-Fu Tang|2022|Dalton Trans.|51|1041|doi:10.1039/D1DT03596G
DOI: 10.5517/ccdc.csd.cc287flk
title: CCDC 2092518: Experimental Crystal Structure Determination

description: Related Article: Xiaomin Hou, Si-Fu Tang|2022|Dalton Trans.|51|1041|doi:10.1039/D1DT03596G
DOI: 10.5517/ccdc.csd.cc287fml
title: CCDC 2092519: Experimental Crystal Structure Determination

description: Related Article: Xiaomin Hou, Si-Fu Tang|2022|Dalton Trans.|51|1041|doi:10.1039/D1DT03596G
DOI: 10.5517/ccdc.csd.cc287fnm
title: CCDC 2092520: Experimental Crystal Structure Determination

description: Related Article: Xiaomin Hou, Si-Fu Tang|2022|Dalton Trans.|51|1041|doi:10.1039/D1DT03596G
DOI: 10.5066/p90m04st
title: Permafrost characterization at the Alaska Peatland Experiment (APEX) site: Geophysical and related field data collected from 2018-2020

description: Geophysical measurements and related field data were collected by the U.S. Geological Survey (USGS) at the Alaska Peatland Experiment (APEX) site in Interior Alaska from 2018 to 2020 to characterize subsurface thermal and hydrologic conditions along a permafrost thaw gradient. The APEX site is managed by the Bonanza Creek LTER (Long Term Ecological Research). In April 2018, seven boreholes were emplaced to depths of 2.3-2.5 meters (m) to allow for repeat logging with downhole nuclear magnetic resonance (NMR) to quantify the spatial and temporal variations in unfrozen water content within active-layer and permafrost soils. NMR data were collected on ten separate occasions between April 2018 and October 2020. In June 2018, soil temperature and moisture sensors were installed at select locations and depths across the study site to record point-scale temperature and moisture conditions in 30 minute intervals. In August 2018, electrical resistivity tomography (ERT) data were collected along four 82 m-long transects. Models of electrical resistivity produced from these data revealed the spatial variability in soil lithology and thermal state (frozen vs. thawed) to depths up to 10-15 m below the surface. Lastly, manual permafrost-probe measurements of thaw depths were collected at each instrument location during summer site visits for comparison to the geophysical data.
DOI: 10.5066/p9tll89e
title: Principal facts of regional gravity data in northeast Iowa

description: Gravity data were collected from 2016 through 2018 to assist in mapping subsurface geology in northeastern Iowa. This data release provides principal facts for 1080 new gravity stations that were acquired to supplement existing public gravity data coverage. References cited: Blakely, R.J., 1995, Potential Theory in Gravity and Magnetic Applications, Cambridge University Press, 441 p. International Association of Geodesy, 1971, Geodetic reference system 1967: International Association of Geodesy Special Publication No. 3, 116 p. Morelli, C., ed., 1974, the International gravity standardization net 1971: International Association of Geodesy Special Publication no.4, 194 p. Plouff, Donald, 1977, Preliminary documentation for a FORTRAN program to compute gravity terrain correctionsbased on topography digitized on a geographic grid: U.S. Geological Survey Open-File Report 77-535, 45 p., https://doi.org/10.3133/ofr77535.
DOI: 10.5066/p9iatnbd
title: Principal facts of regional gravity data in the central Upper Peninsula, Michigan, and northeastern Wisconsin

description: Gravity data were collected from 2016 through 2019 to assist in mapping surface and subsurface geology in the central Upper Peninsula of Michigan and in neighboring northeastern Wisconsin. This data release provides principal facts for 1536 new gravity stations that were acquired to supplement existing public gravity data coverage.
DOI: 10.5066/f7jd4twt
title: Prospect- and Mine-Related Features from U.S. Geological Survey 7.5- and 15-Minute Topographic Quadrangle Maps for the Western United States

description: This data release has been updated in 2017 with a newer version that includes additional states. It is recommended to use the updated data and map services of the new data release located at: https://doi.org/10.5066/F78W3CHG These data are part of a larger USGS project to develop an updated geospatial database of mines, mineral deposits and mineral regions in the United States. Mine and prospect-related symbols, such as those used to represent prospect pits, mines, adits, dumps, tailings, etc., hereafter referred to as mine symbols or features, are currently being digitized on a state-by-state basis from the 7.5-minute (1:24, 000-scale) and the 15-minute (1:48, 000 and 1:62,500-scale) archive of the USGS Historical Topographic Maps Collection, or acquired from available databases (California and Nevada, 1:24,000-scale only). Compilation of these features is the first phase in capturing accurate locations and general information about features related to mineral resource exploration and extraction across the U.S. To date, the compilation of 400,000-plus point and polygon mine symbols from approximately 51,000 maps of 17 western states (AZ, CA, CO,ID, KS, MT, ND, NE, NM, NV, OK, OR, SD, UT, WA, WY and western TX) has been completed. The process renders not only a more complete picture of exploration and mining in the western U.S., but an approximate time line of when these activities occurred. The data may be used for land use planning, assessing abandoned mine lands and mine-related environmental impacts, assessing the value of mineral resources from Federal, State and private lands, and mapping mineralized areas and systems for input into the land management process. The data are presented as three groups of layers based on the scale of the source maps. No reconciliation between the data groups was done.
DOI: 10.6084/m9.figshare.12401168.v18
title: The Brain Hierarchy Score

description: Here we provide data used in Nonaka, Majima, Aoki, & Kamitani (2021) Brain hierarchy score: Which deep neural networks are hierarchically brain-like? <i>iScience</i>.<br><br>See also https://github.com/KamitaniLab/BHscore.<br><br>History:<br><br>2021-12-24 Add encoding accuracy data (encoding_accuracy.zip)<br><br>2020-08-08 Add DNN unit activation data (features-*.zip)<br><br>2020-08-03 Update directory organization in decoding_accuracy.zip<br>
DOI: 10.6084/m9.figshare.18393032.v1
title: Additional file 1 of Did you hear about HIV self-testing? HIV self-testing awareness after community-based HIVST distribution in rural Zimbabwe

description: Additional file 1. Household questionnaire Zimbabwe.
DOI: 10.6084/m9.figshare.18393032
title: Additional file 1 of Did you hear about HIV self-testing? HIV self-testing awareness after community-based HIVST distribution in rural Zimbabwe

description: Additional file 1. Household questionnaire Zimbabwe.
DOI: 10.6084/m9.figshare.18864610
title: Additional file 2 of Performance of Swedish Warmblood fragile foal syndrome carriers and breeding prospects

description: Additional file 2: Table S1. Descriptive statistics of the traditional evaluating traits in the NS horses. The following values are reported for each traditional evaluating trait in the NS horses: number of observations, mean, standard deviation, minimum, 25th percentile, 75th percentile and maximum.
DOI: 10.6084/m9.figshare.18864610.v1
title: Additional file 2 of Performance of Swedish Warmblood fragile foal syndrome carriers and breeding prospects

description: Additional file 2: Table S1. Descriptive statistics of the traditional evaluating traits in the NS horses. The following values are reported for each traditional evaluating trait in the NS horses: number of observations, mean, standard deviation, minimum, 25th percentile, 75th percentile and maximum.
DOI: 10.6084/m9.figshare.18864613.v1
title: Additional file 3 of Performance of Swedish Warmblood fragile foal syndrome carriers and breeding prospects

description: Additional file 3: Table S2. Effect of the WFFS genotype on the DEBV for the linear descriptive traits for both NS and SJ SWB horses. Table S2 shows the effect of the WFFS expressed in significance level and in LSM of the DEBV for the linear descriptive traits per each subgroup (NS and SJ SWB). EBV for the linear descriptive traits in the SWB population have a mean value of 100 and a genetic standard deviation of 4 index units.
DOI: 10.6084/m9.figshare.18864613
title: Additional file 3 of Performance of Swedish Warmblood fragile foal syndrome carriers and breeding prospects

description: Additional file 3: Table S2. Effect of the WFFS genotype on the DEBV for the linear descriptive traits for both NS and SJ SWB horses. Table S2 shows the effect of the WFFS expressed in significance level and in LSM of the DEBV for the linear descriptive traits per each subgroup (NS and SJ SWB). EBV for the linear descriptive traits in the SWB population have a mean value of 100 and a genetic standard deviation of 4 index units.
DOI: 10.6084/m9.figshare.18864616.v1
title: Additional file 4 of Performance of Swedish Warmblood fragile foal syndrome carriers and breeding prospects

description: Additional file 4: Table S3. Descriptive statistics of the traditional evaluating traits in the SJ horses. The following values are reported for each traditional evaluating trait in the SJ horses: number of observations, mean, standard deviation, minimum, 25th percentile, 75th percentile and maximum.
DOI: 10.6084/m9.figshare.18864616
title: Additional file 4 of Performance of Swedish Warmblood fragile foal syndrome carriers and breeding prospects

description: Additional file 4: Table S3. Descriptive statistics of the traditional evaluating traits in the SJ horses. The following values are reported for each traditional evaluating trait in the SJ horses: number of observations, mean, standard deviation, minimum, 25th percentile, 75th percentile and maximum.
DOI: 10.6084/m9.figshare.18864650
title: Additional file 2 of Different pancreatic cancer microenvironments convert iPSCs into cancer stem cells exhibiting distinct plasticity with altered gene expression of metabolic pathways

description: Additional file 2: Supplementary Table 2
DOI: 10.6084/m9.figshare.18864647
title: Additional file 1 of Different pancreatic cancer microenvironments convert iPSCs into cancer stem cells exhibiting distinct plasticity with altered gene expression of metabolic pathways

description: Additional file 1: Supplementary Table 1
DOI: 10.6084/m9.figshare.18864647.v1
title: Additional file 1 of Different pancreatic cancer microenvironments convert iPSCs into cancer stem cells exhibiting distinct plasticity with altered gene expression of metabolic pathways

description: Additional file 1: Supplementary Table 1
DOI: 10.6084/m9.figshare.18864650.v1
title: Additional file 2 of Different pancreatic cancer microenvironments convert iPSCs into cancer stem cells exhibiting distinct plasticity with altered gene expression of metabolic pathways

description: Additional file 2: Supplementary Table 2
DOI: 10.6084/m9.figshare.18864653.v1
title: Additional file 3 of Different pancreatic cancer microenvironments convert iPSCs into cancer stem cells exhibiting distinct plasticity with altered gene expression of metabolic pathways

description: Additional file 3: Supplementary Table 3
DOI: 10.6084/m9.figshare.18864656
title: Additional file 4 of Different pancreatic cancer microenvironments convert iPSCs into cancer stem cells exhibiting distinct plasticity with altered gene expression of metabolic pathways

description: Additional file 4: Supplementary Table 5
DOI: 10.6084/m9.figshare.18864653
title: Additional file 3 of Different pancreatic cancer microenvironments convert iPSCs into cancer stem cells exhibiting distinct plasticity with altered gene expression of metabolic pathways

description: Additional file 3: Supplementary Table 3
DOI: 10.6084/m9.figshare.18864656.v1
title: Additional file 4 of Different pancreatic cancer microenvironments convert iPSCs into cancer stem cells exhibiting distinct plasticity with altered gene expression of metabolic pathways

description: Additional file 4: Supplementary Table 5