豫西老庙沟斑岩-矽卡岩型钼矿床花岗斑岩脉成因、辉钼矿Re-Os年龄及其地质意义

	周栋; 金昌; 高昕宇; 赵太平; 包志伟; 姚军明
	豫西老庙沟斑岩-矽卡岩型钼矿床花岗斑岩脉成因、辉钼矿Re-Os年龄及其地质意义
Source Publication	大地构造与成矿学
ISSN	1001-1552
	2018
Volume	42 Issue:03 Pages:534-549
DOI	10.16539/j.ddgzyckx.2018.03.009
Language	中文
Indexed By	EI
Citation statistics
Document Type	期刊论文
Identifier	http://ir.gig.ac.cn/handle/344008/36383
Collection	中国科学院矿物学与成矿学重点实验室
Recommended Citation GB/T 7714	周栋,金昌,高昕宇,等. 豫西老庙沟斑岩-矽卡岩型钼矿床花岗斑岩脉成因、辉钼矿Re-Os年龄及其地质意义[J]. 大地构造与成矿学,2018,42(03):534-549.
APA	周栋,金昌,高昕宇,赵太平,包志伟,&姚军明.(2018).豫西老庙沟斑岩-矽卡岩型钼矿床花岗斑岩脉成因、辉钼矿Re-Os年龄及其地质意义.大地构造与成矿学,42(03),534-549.
MLA	周栋,et al."豫西老庙沟斑岩-矽卡岩型钼矿床花岗斑岩脉成因、辉钼矿Re-Os年龄及其地质意义".大地构造与成矿学 42.03(2018):534-549.

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