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= The Cedars ultramafic mass, Sonoma County, California =
{"@context": "https://schema.org", "@type": "CreativeWork", "additionalType": "USGS Numbered Series", "name": "The Cedars ultramafic mass, Sonoma County, California", "identifier": [{"@type": "PropertyValue", "propertyID": "USGS Publications Warehouse IndexID", "value": "ofr20121164", "url": "https://pubs.usgs.gov/publication/ofr20121164"}, {"@type": "PropertyValue", "propertyID": "USGS Publications Warehouse Internal ID", "value": 70039464}, {"@type": "PropertyValue", "propertyID": "DOI", "value": "10.3133/ofr20121164", "url": "https://doi.org/10.3133/ofr20121164"}], "inLanguage": "en", "isPartOf": [{"@type": "CreativeWorkSeries", "name": "Open-File Report"}], "datePublished": "2012", "dateModified": "2018-06-18", "abstract": "The Cedars ultramafic mass is a mantle fragment that consists of partially serpentinized spinel harzburgite and dunite. Compositional layering and a chromite lineation define a penetrative metamorphic foliation that almost certainly formed in the upper mantle. Although detailed petrofabric and mineral chemistry are presently lacking, it seems reasonable that the Cedars peridotite represents a slice of mantle tectonite that once formed the base of the Coast Range ophiolite, and not an abyssal peridotite tectonically emplaced within the Franciscan accretionary prism.", "description": "iii, 13 p.; maps col.; Plate: 1 Sheet: 15 x 15 inches", "publisher": {"@type": "Organization", "name": "U.S. Geological Survey"}, "author": [{"@type": "Person", "name": "Wentworth, Carl M. cwent@usgs.gov", "givenName": "Carl M.", "familyName": "Wentworth", "email": "cwent@usgs.gov", "identifier": {"@type": "PropertyValue", "propertyID": "ORCID", "value": "0000-0003-2569-569X", "url": "https://orcid.org/0000-0003-2569-569X"}, "affiliation": [{"@type": "Organization", "name": "Geology, Minerals, Energy, and Geophysics Science Center", "url": "https://www.usgs.gov/centers/gmeg"}]}, {"@type": "Person", "name": "Bailey, Edgar H.", "givenName": "Edgar H.", "familyName": "Bailey"}, {"@type": "Person", "name": "Blake, M. Clark Jr.", "givenName": "M. Clark", "familyName": "Blake"}], "funder": [{"@type": "Organization", "name": "Geology, Minerals, Energy, and Geophysics Science Center", "url": "https://www.usgs.gov/centers/gmeg"}], "spatialCoverage": [{"@type": "Place", "additionalType": "country", "name": "United States", "url": "https://geonames.org/6252001"}, {"@type": "Place", "additionalType": "state", "name": "California", "url": "https://geonames.org/5332921"}, {"@type": "Place", "additionalType": "state", "name": "Sonoma County", "url": "https://geonames.org/5397100"}]}
The Cedars ultramafic mass is a mantle fragment that consists of partially serpentinized spinel harzburgite and dunite. Compositional layering and a chromite lineation define a penetrative metamorphic foliation that almost certainly formed in the upper mantle. Although detailed petrofabric and mineral chemistry are presently lacking, it seems reasonable that the Cedars peridotite represents a slice of mantle tectonite that once formed the base of the Coast Range ophiolite, and not an abyssal peridotite tectonically emplaced within the Franciscan accretionary prism.