Item talk:Q330779: Difference between revisions

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{
{
   "id": "10.5066/p9ouffks",
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Line 118: Line 117:
     "published": "2021",
     "published": "2021",
     "updated": "2021-08-17T11:26:28.000Z"
     "updated": "2021-08-17T11:26:28.000Z"
   },
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}
}

Latest revision as of 00:54, 11 September 2024

{ 

 "DOI": {
   "doi": "10.5066/p9ouffks",
   "prefix": "10.5066",
   "suffix": "p9ouffks",
   "identifiers": [],
   "alternateIdentifiers": [],
   "creators": [
     {
       "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"
         }
       ]
     },
     {
       "name": "McLaughlin, Robert J",
       "nameType": "Personal",
       "givenName": "Robert J",
       "familyName": "McLaughlin",
       "affiliation": [],
       "nameIdentifiers": []
     },
     {
       "name": "Lienkaemper, James J",
       "nameType": "Personal",
       "givenName": "James J",
       "familyName": "Lienkaemper",
       "affiliation": [],
       "nameIdentifiers": [
         {
           "schemeUri": "https://orcid.org",
           "nameIdentifier": "https://orcid.org/0000-0002-7578-7042",
           "nameIdentifierScheme": "ORCID"
         }
       ]
     }
   ],
   "titles": [
     {
       "title": "Data for \"Serpentinite-rich Gouge in a Creeping Segment of the Bartlett Springs Fault, Northern California: Comparison with SAFOD and Implications for Seismic Hazard\""
     }
   ],
   "publisher": "U.S. Geological Survey",
   "container": {},
   "publicationYear": 2021,
   "subjects": [
     {
       "subject": "Mineralogy,Structural Geology"
     }
   ],
   "contributors": [],
   "dates": [
     {
       "date": "2021",
       "dateType": "Issued"
     }
   ],
   "language": null,
   "types": {
     "ris": "DATA",
     "bibtex": "misc",
     "citeproc": "dataset",
     "schemaOrg": "Dataset",
     "resourceType": "Dataset",
     "resourceTypeGeneral": "Dataset"
   },
   "relatedIdentifiers": [
     {
       "relationType": "IsCitedBy",
       "relatedIdentifier": "10.1029/2018tc005307",
       "relatedIdentifierType": "DOI"
     }
   ],
   "relatedItems": [],
   "sizes": [],
   "formats": [],
   "version": null,
   "rightsList": [],
   "descriptions": [
     {
       "description": "This report presents the mineral chemistry dataset that was used in a published study of serpentinite-rich gouge from an actively creeping trace of the Bartlett Springs Fault in northern California. The fault gouge consists of porphyroclasts of antigorite serpentinite, talc, chlorite, and tremolite-actinolite in a sheared matrix of the same materials. The compositions of spinels in the serpentinite clasts (Table S1) indicate a forearc-peridotite origin for the serpentinite, consistent with a source in the Coast Range ophiolite. The other major minerals in both the porphyroclasts and matrix were analyzed (Table S2) for comparison with serpentinite-bearing gouge from the creeping section of the San Andreas Fault. Table S3 presents serpentine mineral compositions from outcrops of the Coast Range Ophiolite located away from the fault.",
       "descriptionType": "Abstract"
     }
   ],
   "geoLocations": [],
   "fundingReferences": [],
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   "created": "2021-08-17T11:26:24.000Z",
   "registered": "2021-08-17T11:26:28.000Z",
   "published": "2021",
   "updated": "2021-08-17T11:26:28.000Z"
 }

}

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