Late Cretaceous (ca. 90 Ma) adakitic intrusive rocks in the Kelu area, Gangdese Belt (southern Tibet): Slab melting and implications for Cu–Au mineralization

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Late Cretaceous (ca. 90 Ma) adakitic intrusive rocks in the Kelu area, Gangdese Belt (southern Tibet): Slab melting and implications for Cu–Au mineralization

The Gangdese Belt in southern Tibet (GBST) is a major Cu–Au–Mo mineralization zone that mostly formed after the India–Asia collision in association with the small-volume, though widespread, Miocene(18–10 Ma) adakitic porphyries. Cu–Au mineralization has scarcely been found in the regional Jurassic–E...

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Bibliographic Details
Main Authors:	Jiang, Z., Wang, Q., Li, Zheng-Xiang, Wyman, D., Tang, G., Jia, X., Yang, Y.
Format:	Journal Article
Published:	Pergamon-Elsevier Science Ltd 2012
Subjects:	Cu–Au mineralization slab melting adakite Tibet Gangdese arc
Online Access:	http://hdl.handle.net/20.500.11937/12864

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