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Partial melting of the South Qinling orogenic crust, China: Evidence from Triassic migmatites and diorites of the Foping dome
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文摘

Migmatization of lower crustal section took place in ~ 215 Ma in the South Qinling orogen.

Neoproterozoic basement and Mesozoic juvenile rocks underwent strong reworking.

Partial melting and crustal doming related to the post-collisional extension.

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