蒙古中部Tariat新生代玄武岩的地幔源区特征:橄榄石成分及Sr-Nd-Pb同位素证据

	张庆霖[1,2]; 任钟元[1]; 张乐[1]; 张磊[1,2]
	蒙古中部Tariat新生代玄武岩的地幔源区特征:橄榄石成分及Sr-Nd-Pb同位素证据
Source Publication	地球化学
ISSN	0379-1726
	2022
Volume	51 Issue:4 Pages:472-491
Language	中文
Indexed By	CSCD
Citation statistics
Document Type	期刊论文
Identifier	http://ir.gig.ac.cn/handle/344008/68704
Collection	同位素地球化学国家重点实验室
Affiliation	1.中国科学院广州地球化学研究所,同位素地球化学国家重点实验室,广东广州510640 2.中国科学院大学,北京100049
Recommended Citation GB/T 7714	张庆霖[1,2],任钟元[1],张乐[1],等. 蒙古中部Tariat新生代玄武岩的地幔源区特征:橄榄石成分及Sr-Nd-Pb同位素证据[J]. 地球化学,2022,51(4):472-491.
APA	张庆霖[1,2],任钟元[1],张乐[1],&张磊[1,2].(2022).蒙古中部Tariat新生代玄武岩的地幔源区特征:橄榄石成分及Sr-Nd-Pb同位素证据.地球化学,51(4),472-491.
MLA	张庆霖[1,2],et al."蒙古中部Tariat新生代玄武岩的地幔源区特征:橄榄石成分及Sr-Nd-Pb同位素证据".地球化学 51.4(2022):472-491.

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