☆ 4.7 Article

Low-δ18OA-type granites in SW China: Evidence for the interaction between the subducted Paleotethyan slab and the Emeishan mantle plume

GEOLOGICAL SOCIETY OF AMERICA BULLETIN (2022)

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Low-δ18OA-type granites in SW China: Evidence for the interaction between the subducted Paleotethyan slab and the Emeishan mantle plume

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