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- W1994080213 abstract "In the packets of tectonic slices there are preserved large-size fragments of Late Precambrian-Early Paleozoic, Late Paleozoic-Triassic, Late Jurassic-Valanginian, Albian-Campanian, and Late Cretaceous ophiolite suites developed in both oceanic and marginal (back-arc) basins. Same belts (or zones) of ophiolites often comprise fragments of different-age complexes. In the Paleozoic ophiolites which, judging from the volcanic series compositions, were formed in different paleo-oceanic environments, mafic complexes are the thickest and include gabbro-norite and gabbro-troctolite series; they are associated with less depleted metamorphic peridotite complexes (lherzolite and pyroxene-rich harzburgite). Marginal basin ophiolites of Late Jurassic-Valanginian age incorporate thin mafic rock bodies of gabbro-norite composition; they are associated with lherzolites, pyroxene-rich harzburgites, olivine-rich harzburgites, and major dunite bodies. Petrochemical types of metamorphic peridotite massifs are given and it is assumed that the latter are fragments of an ancient peridotite layer which throughout the Phanerozoic served as the mantle basement for the crust of oceanic or marginal basins occurring in the northwestern Paleo-Pacific." @default.
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- W1994080213 date "1986-08-01" @default.
- W1994080213 modified "2023-09-26" @default.
- W1994080213 title "Ophiolite belts in the Koryak Upland, Northeast Asia" @default.
- W1994080213 cites W2016165298 @default.
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- W1994080213 doi "https://doi.org/10.1016/0040-1951(86)90069-7" @default.
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