Item talk:Q61944: Difference between revisions
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{ | |||
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. | "USGS Publications Warehouse": { | ||
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"name": "The Cedars ultramafic mass, Sonoma County, California", | |||
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"value": "ofr20121164", | |||
"url": "https://pubs.usgs.gov/publication/ofr20121164" | |||
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"value": "10.3133/ofr20121164", | |||
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"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", | |||
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Latest revision as of 01:00, 15 August 2024
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