Triassic mafic and intermediate magmatism associated with continental collision between the North and South China Cratons in the Korean Peninsula
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文摘

Mafic and intermediate magmatism may have occurred during post-collisional setting.

The magma source of these rocks appears to be the enriched sub-continental lithospheric mantle (SCLM).

This lithospheric mantle is comparable to the SCLM of the southern margin of the North China Craton.

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