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The geochemistry and geochronology of the Xiarihamu II mafic-ultramafic complex, Eastern Kunlun, Qinghai Province, China: Implications for the genesis of magmatic Ni-Cu sulfide deposits
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文摘

Xiarihamu is the first large Cu–Ni magmatic deposit discovered in Eastern Kunlun, Qinghai Province, China.

Xiarihamu II mafic–ultramafic complex has a close temporal relationship with the mineralization.

The complex probably formed in a post-collisional, extensional regime.

Earlier enrichment of the lithospheric mantle aided the generation of mafic magma, eventually forming the complex and deposit.

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