新疆阿尔泰三叠纪锂矿化伟晶岩中热液成矿作用：来自单个流体包裹体组成LA-ICP-MS原位分析证据

	新疆阿尔泰三叠纪锂矿化伟晶岩中热液成矿作用：来自单个流体包裹体组成LA-ICP-MS原位分析证据
	郭柳 ; 张辉 ; 吕正航; 唐勇 ; 安燚 ; 陈剑争
	2023
Source Publication	矿物学报
Volume	43 Issue:1 Pages:25-37
DOI	10.16461/j.cnki.1000-4734.2022.42.077
Indexed By	CSCD
Language	中文
CSCD ID	CSCD:7509816
Citation statistics	Cited Times:1[CSCD] [CSCD Record]
Document Type	期刊论文
Identifier	http://ir.gyig.ac.cn/handle/42920512-1/14094
Collection	地球内部物质高温高压实验室地球深部物质与流体作用地球化学研究室
Affiliation	1.中国科学院地球化学研究所地球内部物质与高温高压院重点实验室 2.中国科学院大学
Recommended Citation GB/T 7714	郭柳,张辉,吕正航,等. 新疆阿尔泰三叠纪锂矿化伟晶岩中热液成矿作用：来自单个流体包裹体组成LA-ICP-MS原位分析证据[J]. 矿物学报,2023,43(1):25-37.
APA	郭柳,张辉,吕正航,唐勇,安燚,&陈剑争.(2023).新疆阿尔泰三叠纪锂矿化伟晶岩中热液成矿作用：来自单个流体包裹体组成LA-ICP-MS原位分析证据.矿物学报,43(1),25-37.
MLA	郭柳,et al."新疆阿尔泰三叠纪锂矿化伟晶岩中热液成矿作用：来自单个流体包裹体组成LA-ICP-MS原位分析证据".矿物学报 43.1(2023):25-37.

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