Item talk:Q318095
From geokb
{
"DOI": { "doi": "10.5066/p9qh5zyp", "identifiers": [], "creators": [ { "name": "Wintzer, Niki E", "nameType": "Personal", "givenName": "Niki E", "familyName": "Wintzer", "affiliation": [], "nameIdentifiers": [ { "schemeUri": "https://orcid.org", "nameIdentifier": "https://orcid.org/0000-0003-3085-435X", "nameIdentifierScheme": "ORCID" } ] }, { "name": "Schmitz, Mark D.", "nameType": "Personal", "givenName": "Mark D.", "familyName": "Schmitz", "affiliation": [], "nameIdentifiers": [] }, { "name": "Gillerman, Virginia S.", "nameType": "Personal", "givenName": "Virginia S.", "familyName": "Gillerman", "affiliation": [], "nameIdentifiers": [] }, { "name": "Vervoort, Jeffrey D.", "nameType": "Personal", "givenName": "Jeffrey D.", "familyName": "Vervoort", "affiliation": [], "nameIdentifiers": [] } ], "titles": [ { "title": "Isotopic ratios and element concentrations of U-Pb and Sm-Nd for scheelite petrochronology" } ], "publisher": "U.S. Geological Survey", "container": {}, "publicationYear": 2020, "subjects": [ { "subject": "Economic Geology, Geochemistry" } ], "contributors": [], "dates": [ { "date": "2020", "dateType": "Issued" } ], "language": null, "types": { "ris": "DATA", "bibtex": "misc", "citeproc": "dataset", "schemaOrg": "Dataset", "resourceType": "Dataset", "resourceTypeGeneral": "Dataset" }, "relatedIdentifiers": [ { "relationType": "IsCitedBy", "relatedIdentifier": "10.5382/econgeo.4953", "relatedIdentifierType": "DOI" } ], "relatedItems": [], "sizes": [], "formats": [], "version": null, "rightsList": [], "descriptions": [ { "description": "Instrument, standard, and sample data from application of in situ laser ablation-inductively coupled plasma-mass spectrometry (LA-ICPMS) dating of scheelite in thin section, and sample data from isotope dilution thermal ionization mass spectrometry (ID-TIMS) scheelite dating are in this data release. Fractionation factor and ratio data in between NIST glass and natural scheelite as well as isotope dilution Sm-Nd scheelite data are also included. Scheelite is from two ore deposits within the Stibnite-Yellow Pine mining area, and analyses yielded bimodal U-Pb ages with major growth of scheelite in the range of 61.3 +- 4.1 to 55.1 +- 3.8 Ma and a second growth event involving both scheelite and stibnite at 45.8 +- 2.6 Ma. In situ analyses were calibrated and confirmed by ID-TIMS U-Pb lower intercept ages of two coarsely crystalline scheelite samples yielded ages of 56.62 +- 0.16 Ma and 57.52 +- 0.22 Ma. These results, in good agreement with 40Ar/39Ar ages of 57.08 +- 0.12 to 56.2 +- 1.2 Ma from adularia petrographically linked to scheelite, confirm primary scheelite mineralization occurred ca. 57.5 Ma. This geochronology resolves a long-standing debate about the formation age of scheelite and stibnite within the United States' largest antimony source. Calibration with ID-TIMS provided reliable ages, and crystals from the same sample were used as a matrix-matched primary standard material for LA-ICPMS. No matrix-match standard was previously characterized accentuating the importance of this newly characterized matrix-matched scheelite standard.", "descriptionType": "Abstract" } ], "geoLocations": [], "fundingReferences": [], "url": "https://www.sciencebase.gov/catalog/item/5ef247fb82ced62aaae3bc40", "contentUrl": null, "metadataVersion": 2, "schemaVersion": "http://datacite.org/schema/kernel-4", "source": "mds", "isActive": true, "state": "findable", "reason": null, "viewCount": 0, "downloadCount": 0, "referenceCount": 0, "citationCount": 2, "partCount": 0, "partOfCount": 0, "versionCount": 0, "versionOfCount": 0, "created": "2020-07-29T23:20:58Z", "registered": "2020-07-29T23:20:59Z", "published": null, "updated": "2024-08-10T08:55:20Z" }
}