Item talk:Q302643
From geokb
{
"USGS Publications Warehouse": { "@context": "https://schema.org", "@type": "Article", "additionalType": "Journal Article", "name": "Late Cenozoic volcanism, geochronology, and structure of the Coso Range, Inyo County, California", "identifier": [ { "@type": "PropertyValue", "propertyID": "USGS Publications Warehouse IndexID", "value": "70200638", "url": "https://pubs.usgs.gov/publication/70200638" }, { "@type": "PropertyValue", "propertyID": "USGS Publications Warehouse Internal ID", "value": 70200638 }, { "@type": "PropertyValue", "propertyID": "DOI", "value": "10.1029/JB085iB05p02381", "url": "https://doi.org/10.1029/JB085iB05p02381" } ], "journal": { "@type": "Periodical", "name": "Journal of Geophysical Research B: Solid Earth", "volumeNumber": "85", "issueNumber": "B5" }, "inLanguage": "en", "isPartOf": [ { "@type": "CreativeWorkSeries", "name": "Journal of Geophysical Research B: Solid Earth" } ], "datePublished": "1980", "dateModified": "2018-10-25", "abstract": "The Coso Range lies at the west edge of the Great Basin, adjacent to the southern part of the Sierra Nevada. A basement complex of pre\u2010Cenozoic plutonic and metamorphic rocks is partly buried by \u223c35 km3\u00a0of late Cenozoic volcanic rocks that were erupted during two periods, as defined by K\u2010Ar dating: (1) 4.0\u20132.5 m.y., \u223c31 km3\u00a0of basalt, rhyodacite, dacite, andesite, and rhyolite, in descending order of abundance, and (2) \u22641.1 m.y., nearly equal amounts of basalt and rhyolite, most of the rhyolite being \u22640.3 m.y. old. Vents for the volcanic rocks of the younger period are localized on and near a horst of basement rocks within a concavity defined by the distribution of vents of the older period. The alignment of many vents and the presence of a considerable number of roughly north\u2010trending normal faults of late Cenozoic age reflect basin and range tectonics dominated by roughly east\u2010west lithospheric extension. Fumaroles, intermittently active thermal springs, and associated altered rocks occur within and immediately east of the central part of the field of Quaternary rhyolite, in an area characterized by various geophysical anomalies that are evidently related to an active hot\u2010water geothermal system. This system apparently is heated by a reservoir of silicic magma at \u22658\u2010km depth, itself produced and sustained through partial melting of crustal rocks by thermal energy contained in mantle\u2010derived basaltic magma that intrudes the crust in response to lithospheric extension.", "description": "24 p.", "publisher": { "@type": "Organization", "name": "American Geophysical Union" }, "author": [ { "@type": "Person", "name": "Duffield, Wendell A.", "givenName": "Wendell A.", "familyName": "Duffield" }, { "@type": "Person", "name": "Bacon, Charles R. cbacon@usgs.gov", "givenName": "Charles R.", "familyName": "Bacon", "email": "cbacon@usgs.gov", "identifier": { "@type": "PropertyValue", "propertyID": "ORCID", "value": "0000-0002-2165-5618", "url": "https://orcid.org/0000-0002-2165-5618" }, "affiliation": [ { "@type": "Organization", "name": "Volcano Science Center", "url": "https://www.usgs.gov/centers/volcano-science-center" } ] }, { "@type": "Person", "name": "Dalrymple, G. Brent", "givenName": "G. Brent", "familyName": "Dalrymple" } ], "funder": [ { "@type": "Organization", "name": "Volcano Science Center", "url": "https://www.usgs.gov/centers/volcano-science-center" } ], "spatialCoverage": [ { "@type": "Place", "additionalType": "country", "name": "United States", "url": "https://geonames.org/4074035" }, { "@type": "Place", "additionalType": "state", "name": "California" }, { "@type": "Place", "additionalType": "state", "name": "Inyo" }, { "@type": "Place", "additionalType": "unknown", "name": "Coso Range", "url": "https://geonames.org/5339831" } ] }
}