Item talk:Q326780

{

 "id": "10.5066/p9enrs8u",
 "attributes": {
   "doi": "10.5066/p9enrs8u",
   "identifiers": [],
   "creators": [
     {
       "name": "Downs, Drew T",
       "nameType": "Personal",
       "givenName": "Drew T",
       "familyName": "Downs",
       "affiliation": [],
       "nameIdentifiers": []
     },
     {
       "name": "Stelten, Mark E",
       "nameType": "Personal",
       "givenName": "Mark E",
       "familyName": "Stelten",
       "affiliation": [],
       "nameIdentifiers": [
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           "schemeUri": "https://orcid.org",
           "nameIdentifier": "https://orcid.org/0000-0002-5294-3161",
           "nameIdentifierScheme": "ORCID"
         }
       ]
     }
   ],
   "titles": [
     {
       "title": "Electron microprobe data for plagioclase, olivine, pyroxene, and spinel in volcanic rocks from the Matan volcanic center located within the Harrat Rahat volcanic field, Kingdom of Saudi Arabia"
     }
   ],
   "publisher": "U.S. Geological Survey",
   "container": {},
   "publicationYear": 2022,
   "subjects": [],
   "contributors": [],
   "dates": [
     {
       "date": "2022",
       "dateType": "Issued"
     }
   ],
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   "descriptions": [
     {
       "description": "Mineral compositions are reported for Quaternary volcanic rocks of the Matan volcanic center, northern Harrat Rahat, Saudi Arabia. Compositions were measured by wavelength-dispersive methods with the 5-spectrometer JEOL-8900 electron microprobe at the USGS facility in Menlo Park, California; background-corrected X-ray intensities were reduced to oxide weight concentrations with the JEOL proprietary version of the CITZAF reduction schema. These results are part of a collaborative study by the U.S. Geological Survey and Saudi Geological survey to assess the volcanic and seismic hazards associated with the northern Harrat Rahat volcanic field.",
       "descriptionType": "Abstract"
     }
   ],
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   "created": "2022-02-15T17:27:20Z",
   "registered": "2022-02-15T17:27:21Z",
   "published": null,
   "updated": "2022-02-15T17:27:21Z"
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