台湾利吉混杂岩中蛇纹岩伴生碳酸盐岩地球化学特征及其成因分析

GIG OpenIR

	李鸿莉[1]; 冯俊熙[2,3]; 佟宏鹏[1]; 王钦贤[1]; 陈多福[1,2]
	台湾利吉混杂岩中蛇纹岩伴生碳酸盐岩地球化学特征及其成因分析
Source Publication	地球化学
ISSN	0379-1726
	2023
Volume	52 Issue:2 Pages:222-237
Language	中文
Indexed By	CSCD
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Document Type	期刊论文
Identifier	http://ir.gig.ac.cn/handle/344008/70088
Collection	中国科学院广州地球化学研究所
Affiliation	1.上海海洋大学海洋生态与环境学院/海洋科学学院,上海201306 2.中国科学院广州地球化学研究所边缘海与大洋地质重点实验室,广东广州510640 3.中国地质调查局广州海洋地质调查局,广东广州510075
Recommended Citation GB/T 7714	李鸿莉[1],冯俊熙[2,3],佟宏鹏[1],等. 台湾利吉混杂岩中蛇纹岩伴生碳酸盐岩地球化学特征及其成因分析[J]. 地球化学,2023,52(2):222-237.
APA	李鸿莉[1],冯俊熙[2,3],佟宏鹏[1],王钦贤[1],&陈多福[1,2].(2023).台湾利吉混杂岩中蛇纹岩伴生碳酸盐岩地球化学特征及其成因分析.地球化学,52(2),222-237.
MLA	李鸿莉[1],et al."台湾利吉混杂岩中蛇纹岩伴生碳酸盐岩地球化学特征及其成因分析".地球化学 52.2(2023):222-237.

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