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Late Mesozoic (180–70 Ma) lithosphere delamination, asthenosphere upwelling and paleo-Pacific subduction in South China. The asthenosphere upwelling and decompression melting during 180–120 Ma were triggered by the lithospheric delamination, whereas those after 120 Ma were caused by the rollback of the paleo-Pacific subducting slab.
#Illustration#Lithosphere Delamination#Asthenosphere Upwelling#Paleo-Pacific Subduction#Decompression Melting#South China
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