Geochronological and geochemical constraints on genesis of the adakitic rocks in Outang, South Tan-Lu Fault Belt (Northeastern Yangtze Block)
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文摘

Adakitic rocks along South Tan-Lu fault belt formed between 124-129 Ma.

Origin of the adakitic rocks is partial melting of delaminated lower crust.

Crustal materials dominated processing of these igneous rocks.

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