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• W2340449849 abstract "The Upper Jurassic Galice Formation of the Klamath Mountains, Oregon-California, overlies the ca. 162-Ma Josephine ophiolite and the slightly younger Rogue–Chetco volcano-plutonic arc complex. The Galice Formation that overlies the Josephine ophiolite consists of a siliceous hemipelagic sequence, which grades upward into a thick turbidite sequence. Bedded hemipelagic rocks and scarce sandstone, however, also occur at several localities within the Josephine ophiolite pillow basalts. Corrected paleoflow current data suggest that the Galice Formation was derived predominantly from the east and north. Detrital modes of sandstones from the Galice Formation indicate an arc source as well as a predominantly chert-argillite source..." @default.
• W2340449849 created "2016-06-24" @default.
• W2340449849 creator A5030548583 @default.
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• W2340449849 date "2006-01-01" @default.
• W2340449849 modified "2023-10-04" @default.
• W2340449849 title "Petrology, geochemistry, and provenance of the Galice Formation, Klamath Mountains, Oregon and California" @default.
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• W2340449849 doi "https://doi.org/10.1130/2006.2410(04)" @default.
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