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- W2027142016 abstract "A group of peridotites in southwestern Oregon contains high-pressure mineral assemblages reflecting recrystallization at high temperatures (1100 degrees to 1200 degrees C) over a range of pressure decreasing from 19 to 5 kilobars. It is proposed that the peridotites represent upper-mantle material brought from depth along the ancestral Gorda-Juan de Fuca ridge system, transported eastward by the spreading Gorda lithosphere plate, and then emplaced by thrust-faulting in the western margin of the Cordillera during late Mesozoic time." @default.
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- W2027142016 date "1970-09-04" @default.
- W2027142016 modified "2023-09-24" @default.
- W2027142016 title "Mantle-Derived Peridotites in Southwestern Oregon: Relation to Plate Tectonics" @default.
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- W2027142016 doi "https://doi.org/10.1126/science.169.3949.971" @default.
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