大陆内部浆控高温热液矿床成矿流体性质及其与岛弧区同类矿床的差异

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	陈衍景; 李诺
	大陆内部浆控高温热液矿床成矿流体性质及其与岛弧区同类矿床的差异
Source Publication	岩石学报
ISSN	1000-0569
	2009
Volume	25 Issue:10 Pages:2477-2508
Indexed By	SCI
Document Type	期刊论文
Identifier	http://ir.gig.ac.cn/handle/344008/14779
Collection	中国科学院广州地球化学研究所
Recommended Citation GB/T 7714	陈衍景,李诺. 大陆内部浆控高温热液矿床成矿流体性质及其与岛弧区同类矿床的差异[J]. 岩石学报,2009,25(10):2477-2508.
APA	陈衍景,&李诺.(2009).大陆内部浆控高温热液矿床成矿流体性质及其与岛弧区同类矿床的差异.岩石学报,25(10),2477-2508.
MLA	陈衍景,et al."大陆内部浆控高温热液矿床成矿流体性质及其与岛弧区同类矿床的差异".岩石学报 25.10(2009):2477-2508.

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