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5. Increased Magmatic Water Content-the Key to Porphyry Cu-Mo ± Au Formation in the Gangdese Belt, Tibe

Increased Magmatic Water Content-the Key to Porphyry Cu-Mo ± Au Formation in the Gangdese Belt, Tibe

来源 :The First Joint Scientific Meeting of Geological Society of | 被引量 : 0次 | 上传用户：zhqimin

【作 者】

：

WANG Rui RICHARDS Jeremy HOU Zengqian YANG Zhiming 

【机 构】

：

Department of Earth and Atmospheric Sciences, University of Alberta, Edmonton, Alberta, Canada, T6G

【出 处】

：

The First Joint Scientific Meeting of Geological Society of

【发表日期】

：

2013年11期

【关键词】

：

magmatic water porphyry deposit Miocene Oligocene Eocene Gangdese Tibet Hornblen 

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