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Slab-derived adakites and subslab asthenosphere-derived OIB-type rocks at 156 ± 2 Ma from the north of Gerze, central Tibet: Records of the Bangong-Nujiang oceanic ridge subduction during the Late Jurassic
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文摘

The presence of a distinct rock association of coeval adakitic dacites and OIB-type rocks

Subducting oceanic slab and upwelling subslab asthenosphere are proposed to explain their generation, respectively.

Northward subduction of the Tethyan Bangong-Nujiang Ocean ridge during the Late Jurassic

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