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	Zircon Hf-O Isotopes of the Gangdese Porphyry Cu Deposits:Implication for Generation of Porphyry Cu Deposits in Collisional Orogenic Setting; Zircon Hf-O Isotopes of the Gangdese Porphyry Cu Deposits:Implication for Generation of Porphyry Cu Deposits in Collisional Orogenic Setting
	LI Qiuyun ; HOU Zengqian ; YANG Zhiming ; ZHENG Yuanchuan ; YU Feng ; WANG Rui
	2014
关键词	subduction continental mostly island Miocene zircon alkaline dating mantle magmatic subduction continental mostly island Miocene zircon alkaline dating mantle magmatic
英文摘要	1 Introduction Porphyry Cu deposits mostly occur in island-arc and continental arc settings worldwide in association with subduction-related calc-alkaline intermediate-felsic magmas(Richards,2003;Cooke et al,2005;Sillitoe,2010).Recent studies have documented that such deposits also occur in post-subduction setting,such as Miocene; 1 Introduction Porphyry Cu deposits mostly occur in island-arc and continental arc settings worldwide in association with subduction-related calc-alkaline intermediate-felsic magmas(Richards,2003;Cooke et al,2005;Sillitoe,2010).Recent studies have documented that such deposits also occur in post-subduction setting,such as Miocene; 中国地质调查局、国际矿床成因协会; 2; Vol.88
语种	英语
出处	第14届国际矿床成因协会大会
内容类型	其他
源URL	[http://ir.pku.edu.cn/handle/20.500.11897/480248]
专题	地球与空间科学学院
推荐引用方式 GB/T 7714	LI Qiuyun,HOU Zengqian,YANG Zhiming,et al. Zircon Hf-O Isotopes of the Gangdese Porphyry Cu Deposits:Implication for Generation of Porphyry Cu Deposits in Collisional Orogenic Setting, Zircon Hf-O Isotopes of the Gangdese Porphyry Cu Deposits:Implication for Generation of Porphyry Cu Deposits in Collisional Orogenic Setting. 2014-01-01.

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