大兴安岭北段晚中生代斑岩铜钼矿床成矿岩体黑云母地球化学特征及地质意义

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	孟凡波 1; 邓昌州 2; 冯雨周 3; 田振东 2; 李成禄 4; 龚林 3; 陈旭升 1; 吕凤彤 1
	大兴安岭北段晚中生代斑岩铜钼矿床成矿岩体黑云母地球化学特征及地质意义
Source Publication	矿物岩石地球化学通报
ISSN	1007-2802
	2021
Volume	40 Issue:4 Pages:914-924
Language	中文
CSCD ID	CSCD:7121469
Indexed By	CSCD
Citation statistics
Document Type	期刊论文
Identifier	http://ir.gig.ac.cn/handle/344008/63606
Collection	中国科学院广州地球化学研究所
Affiliation	1.黑龙江省齐齐哈尔地质勘查院,黑龙江齐齐哈尔161006; 2.中国科学院地球化学研究所,贵阳550081; 3.中国科学院广州地球化学研究所,广州510640; 4.黑龙江省自然资源调查院,哈尔滨150036
Recommended Citation GB/T 7714	孟凡波,邓昌州,冯雨周,等. 大兴安岭北段晚中生代斑岩铜钼矿床成矿岩体黑云母地球化学特征及地质意义[J]. 矿物岩石地球化学通报,2021,40(4):914-924.
APA	孟凡波.,邓昌州.,冯雨周.,田振东.,李成禄.,...&吕凤彤.(2021).大兴安岭北段晚中生代斑岩铜钼矿床成矿岩体黑云母地球化学特征及地质意义.矿物岩石地球化学通报,40(4),914-924.
MLA	孟凡波,et al."大兴安岭北段晚中生代斑岩铜钼矿床成矿岩体黑云母地球化学特征及地质意义".矿物岩石地球化学通报 40.4(2021):914-924.

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