云南白牛厂银多金属矿床成因

	云南白牛厂银多金属矿床成因
	祝朝辉; 张乾; 邵树勋; 何玉良; 王大鹏
	2006
Source Publication	世界地质
Volume	25 Issue:4 Pages:353-359
metadata_24	其它
Abstract	对云南白牛厂超大型银多金属矿床的地质、地球化学特征厦矿床形成的长期性及多阶段性的研究认为：白牛厂银多金属矿床是热水沉积—叠生成因矿床，早期呈现寒武纪的热水同生沉积成矿作用，晚期为燕山期花岗岩浆热液成矿作用。该矿床是热水沉积成矿作用与岩浆热液成矿作用叠加成矿的产物.
Keyword	云南
Subject Area	中国典型特殊区带大规模成矿作用及其动力学
Funding Organization	中国科学院重点方向项目（KZCW3-SW-125）
Indexed By	CSCD
Language	中文
CSCD ID	CSCD:2644327
Citation statistics	Cited Times:4[CSCD] [CSCD Record]
Document Type	期刊论文
Identifier	http://ir.gyig.ac.cn/handle/352002/559
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	祝朝辉,张乾,邵树勋,等. 云南白牛厂银多金属矿床成因[J]. 世界地质,2006,25(4):353-359.
APA	祝朝辉,张乾,邵树勋,何玉良,&王大鹏.(2006).云南白牛厂银多金属矿床成因.世界地质,25(4),353-359.
MLA	祝朝辉,et al."云南白牛厂银多金属矿床成因".世界地质 25.4(2006):353-359.

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