碳酸盐化榴辉岩对板内碱性玄武岩源区的贡献

	徐荣[1]; 刘勇胜[2]; 张艳飞[2]; 邹宗琪[3]; 张军波[2]
	碳酸盐化榴辉岩对板内碱性玄武岩源区的贡献
Source Publication	岩石学报
ISSN	1000-0569
	2022
Volume	38 Issue:12 Pages:3771-3784
Language	中文
WOS ID	WOS:000826244200010
Indexed By	SCI ; EI ; CSCD
Citation statistics	Cited Times:2[WOS] [WOS Record] [Related Records in WOS]
Document Type	期刊论文
Identifier	http://ir.gig.ac.cn/handle/344008/68740
Collection	同位素地球化学国家重点实验室
Affiliation	1.中国科学院地球化学研究所,矿床地球化学国家重点实验室,贵阳550081 2.中国地质大学(武汉)地球科学学院,地质过程与矿产资源国家重点实验室,武汉430074 3.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,广州510640
Recommended Citation GB/T 7714	徐荣[1],刘勇胜[2],张艳飞[2],等. 碳酸盐化榴辉岩对板内碱性玄武岩源区的贡献[J]. 岩石学报,2022,38(12):3771-3784.
APA	徐荣[1],刘勇胜[2],张艳飞[2],邹宗琪[3],&张军波[2].(2022).碳酸盐化榴辉岩对板内碱性玄武岩源区的贡献.岩石学报,38(12),3771-3784.
MLA	徐荣[1],et al."碳酸盐化榴辉岩对板内碱性玄武岩源区的贡献".岩石学报 38.12(2022):3771-3784.

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