Origin of postcollisional magmas and formation of porphyry Cu deposits in southern Tibet

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Origin of postcollisional magmas and formation of porphyry Cu deposits in southern Tibet

The recent discovery of large porphyry copper deposits (PCDs) associated with Miocene (22–12 Ma) granitoid magmas in the eastern section of the Paleocene-Eocene Gangdese magmatic arc in the Himalaya-Tibetan orogenic belt raises new questions about the origin of water-rich (≥4.5 wt.%), oxidized (ΔFMQ...

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Bibliographic Details
Main Authors:	Wang, R., Weinberg, R., Collins, Bill, Richards, J., Zhu, D.
Format:	Journal Article
Published:	Elsevier BV 2018
Online Access:	http://hdl.handle.net/20.500.11937/66923

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