川西南拉一木玄武岩型铜矿流体包裹体地球化学特征

	川西南拉一木玄武岩型铜矿流体包裹体地球化学特征
	王富东; 朱笑青; 王中刚
	2013
Source Publication	矿物学报
Issue	S2 Pages:496-497
Keyword	流体包裹体铜矿床地球化学特征成矿元素侯增晚古生代壳幔带高均一温度背景值
Subject Area	矿床地球化学
Indexed By	CSCD
Language	中文
Citation statistics
Document Type	期刊论文
Identifier	http://ir.gyig.ac.cn/handle/352002/5497
Collection	矿床地球化学国家重点实验室_矿床地球化学国家重点实验室_期刊论文
Recommended Citation GB/T 7714	王富东,朱笑青,王中刚. 川西南拉一木玄武岩型铜矿流体包裹体地球化学特征[J]. 矿物学报,2013(S2):496-497.
APA	王富东,朱笑青,&王中刚.(2013).川西南拉一木玄武岩型铜矿流体包裹体地球化学特征.矿物学报(S2),496-497.
MLA	王富东,et al."川西南拉一木玄武岩型铜矿流体包裹体地球化学特征".矿物学报 .S2(2013):496-497.

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