江绍断裂带晚中生代镁铁质火山岩成因及其深部过程意义

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	秦社彩; 范蔚茗; 郭锋
	江绍断裂带晚中生代镁铁质火山岩成因及其深部过程意义
Source Publication	岩石学报
ISSN	1000-0569
	2019
Volume	35 Issue:6 Pages:1892-1906
DOI	10.18654/1000-0569/2019.06.16
Language	中文
WOS Research Area	Geology
WOS ID	WOS:000476647200016
Indexed By	SCI
Citation statistics	Cited Times:3[WOS] [WOS Record] [Related Records in WOS]
Document Type	期刊论文
Identifier	http://ir.gig.ac.cn/handle/344008/47119
Collection	中国科学院广州地球化学研究所
Recommended Citation GB/T 7714	秦社彩,范蔚茗,郭锋. 江绍断裂带晚中生代镁铁质火山岩成因及其深部过程意义[J]. 岩石学报,2019,35(6):1892-1906.
APA	秦社彩,范蔚茗,&郭锋.(2019).江绍断裂带晚中生代镁铁质火山岩成因及其深部过程意义.岩石学报,35(6),1892-1906.
MLA	秦社彩,et al."江绍断裂带晚中生代镁铁质火山岩成因及其深部过程意义".岩石学报 35.6(2019):1892-1906.

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