Item talk:Q320617
From geokb
{
"DOI": { "doi": "10.5066/p9knv1j8", "identifiers": [], "creators": [ { "name": "Jeppson, Tamara N", "nameType": "Personal", "givenName": "Tamara N", "familyName": "Jeppson", "affiliation": [ "United States Geological Survey" ], "nameIdentifiers": [] }, { "name": "Lockner, David A", "nameType": "Personal", "givenName": "David A", "familyName": "Lockner", "affiliation": [], "nameIdentifiers": [ { "schemeUri": "https://orcid.org", "nameIdentifier": "https://orcid.org/0000-0001-8630-6833", "nameIdentifierScheme": "ORCID" } ] }, { "name": "Beeler, Nicholas M", "nameType": "Personal", "givenName": "Nicholas M", "familyName": "Beeler", "affiliation": [], "nameIdentifiers": [ { "schemeUri": "https://orcid.org", "nameIdentifier": "https://orcid.org/0000-0002-3397-8481", "nameIdentifierScheme": "ORCID" } ] }, { "name": "Moore, Diane E", "nameType": "Personal", "givenName": "Diane E", "familyName": "Moore", "affiliation": [], "nameIdentifiers": [ { "schemeUri": "https://orcid.org", "nameIdentifier": "https://orcid.org/0000-0002-8641-1075", "nameIdentifierScheme": "ORCID" } ] } ], "titles": [ { "title": "Slide-hold-slide experiments on Westerly Granite at temperatures up to 250 °C" } ], "publisher": "U.S. Geological Survey", "container": {}, "publicationYear": 2023, "subjects": [ { "subject": "Geophysics" }, { "subject": "FOS: Earth and related environmental sciences", "schemeUri": "http://www.oecd.org/science/inno/38235147.pdf", "subjectScheme": "Fields of Science and Technology (FOS)" } ], "contributors": [], "dates": [ { "date": "2023", "dateType": "Issued" } ], "language": null, "types": { "ris": "DATA", "bibtex": "misc", "citeproc": "dataset", "schemaOrg": "Dataset", "resourceType": "Dataset", "resourceTypeGeneral": "Dataset" }, "relatedIdentifiers": [], "relatedItems": [], "sizes": [], "formats": [], "version": null, "rightsList": [], "descriptions": [ { "description": "Laboratory slide-hold-slide tests were conducted in a conventional triaxial deformation configuration on 1-inch diameter cylindrical cores of Westerly granite bisected by a sawcut oriented at 30 degrees from vertical. Tests were conducted at a constant confining pressure of 30 MPa with a 10 MPa pore fluid pressure. The pore fluid was deionized water. Experiments were conducted at temperatures of 22, 100, 200, and 250 degC.", "descriptionType": "Abstract" } ], "geoLocations": [], "fundingReferences": [], "url": "https://www.sciencebase.gov/catalog/item/64946e01d34ef77fcb015250", "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": 0, "partCount": 0, "partOfCount": 0, "versionCount": 0, "versionOfCount": 0, "created": "2023-10-10T15:06:12Z", "registered": "2023-10-10T15:06:13Z", "published": null, "updated": "2023-10-10T15:06:21Z" }
}