The Nadun Cu-Au mineralization, central Tibet: Root of a high sulfidation epithermal deposit

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The Nadun Cu-Au mineralization, central Tibet: Root of a high sulfidation epithermal deposit

A new high sulfidation epithermal Cu–Au occurrence (Nadun) has been discovered adjacent to the Cretaceous Duolong porphyry Cu–Au deposit within the Bangong–Nujiang metallogenic belt, central Tibet. The Nadun Cu–Au mineralization is hosted in a tectonic–hydrothermal breccia with advanced argillic alt...

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Bibliographic Details
Main Authors:	Li, J., Qin, K., Li, G., Evans, Noreen, Zhao, J., Cao, M., Huang, F.
Format:	Journal Article
Published:	Elsevier Science BV 2016
Online Access:	http://hdl.handle.net/20.500.11937/4346

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