Item talk:Q323454: Difference between revisions
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{ | { | ||
" | "DOI": { | ||
"doi": "10.5066/p9xj7fmm", | "doi": "10.5066/p9xj7fmm", | ||
"identifiers": [], | "identifiers": [], | ||
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"published": null, | "published": null, | ||
"updated": "2023-07-15T08:55:35Z" | "updated": "2023-07-15T08:55:35Z" | ||
} | } | ||
} | } |
Latest revision as of 23:16, 10 September 2024
{
"DOI": { "doi": "10.5066/p9xj7fmm", "identifiers": [], "creators": [ { "name": "Magnin, Benjamin P", "nameType": "Personal", "givenName": "Benjamin P", "familyName": "Magnin", "affiliation": [ "United States Geological Survey" ], "nameIdentifiers": [ { "schemeUri": "https://orcid.org", "nameIdentifier": "https://orcid.org/0000-0001-9951-4404", "nameIdentifierScheme": "ORCID" } ] }, { "name": "Anderson, Eric D", "nameType": "Personal", "givenName": "Eric D", "familyName": "Anderson", "affiliation": [], "nameIdentifiers": [ { "schemeUri": "https://orcid.org", "nameIdentifier": "https://orcid.org/0000-0002-0138-6166", "nameIdentifierScheme": "ORCID" } ] } ], "titles": [ { "title": "Gravity data in the Wet Mountains area, southcentral Colorado, 2021 to 2022" } ], "publisher": "U.S. Geological Survey", "container": {}, "publicationYear": 2023, "subjects": [ { "subject": "Geophysics, Gravity" } ], "contributors": [], "dates": [ { "date": "2023", "dateType": "Issued" } ], "language": null, "types": { "ris": "DATA", "bibtex": "misc", "citeproc": "dataset", "schemaOrg": "Dataset", "resourceType": "Dataset", "resourceTypeGeneral": "Dataset" }, "relatedIdentifiers": [ { "relationType": "IsCitedBy", "relatedIdentifier": "10.1029/2022tc007674", "relatedIdentifierType": "DOI" } ], "relatedItems": [], "sizes": [], "formats": [], "version": null, "rightsList": [], "descriptions": [ { "description": "The U.S. Geological Survey (USGS) collected gravity data in the Wet Mountains, CO from September 2021 to July 2022 to compliment newly collected airborne magnetic data for surface and subsurface geologic mapping. A total of 261 measurements were collected across two Ediacaran-Ordovician alkaline complexes (Gem Park and McClure Mountain) and gabbroic outcrops suspected Ediacaran-Ordovician in age. These data supplement existing public gravity data to aid the subsurface interpretation of mapped and concealed Ediacaran-Ordovician alkaline intrusions related to rare earth element (REE) mineralization.", "descriptionType": "Abstract" } ], "geoLocations": [], "fundingReferences": [], "url": "https://www.sciencebase.gov/catalog/item/6340a15ad34e342aee0747ae", "contentUrl": null, "metadataVersion": 1, "schemaVersion": "http://datacite.org/schema/kernel-4", "source": "mds", "isActive": true, "state": "findable", "reason": null, "viewCount": 0, "downloadCount": 0, "referenceCount": 0, "citationCount": 1, "partCount": 0, "partOfCount": 0, "versionCount": 0, "versionOfCount": 0, "created": "2023-01-06T19:26:22Z", "registered": "2023-01-06T19:26:23Z", "published": null, "updated": "2023-07-15T08:55:35Z" }
}