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The timing, origin and T-fO2 crystallization conditions of long-lived magmatism at the Yangla copper deposit, Sanjiang Tethyan orogenic belt: Implications for post-collisional magmatic-hydrothermal ore formation
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文摘

Two distinct epochs of the post-collisional felsic activity are recognized.

The incorporation of upper crustal components reduced fO2 of quartz monzonite porphyry.

Cu-fertile melts are mainly sourced from the Neoproterozoic hydrous lower arc crustal rocks.

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