扬子克拉通西缘新生代幔源钾质-超钾质岩岩浆氧逸度及其对陆内斑岩成矿作用的启示

	扬子克拉通西缘新生代幔源钾质-超钾质岩岩浆氧逸度及其对陆内斑岩成矿作用的启示
	马瑞 ; 黄明亮 ; 胥磊落; 毕献武; 刘龚
	2020
Source Publication	矿物岩石地球化学通报
Pages	794-809
DOI	10.19658/j.issn.1007-2802.2020.39.031
Indexed By	CSCD
Language	中文
CSCD ID	CSCD:6797066
Citation statistics	正在获取... Cited Times:2[CSCD] [CSCD Record]
Document Type	期刊论文
Identifier	http://ir.gyig.ac.cn/handle/42920512-1/12038
Collection	矿床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 2.中国科学院大学
Recommended Citation GB/T 7714	马瑞,黄明亮,胥磊落,等. 扬子克拉通西缘新生代幔源钾质-超钾质岩岩浆氧逸度及其对陆内斑岩成矿作用的启示[J]. 矿物岩石地球化学通报,2020:794-809.
APA	马瑞,黄明亮,胥磊落,毕献武,&刘龚.(2020).扬子克拉通西缘新生代幔源钾质-超钾质岩岩浆氧逸度及其对陆内斑岩成矿作用的启示.矿物岩石地球化学通报,794-809.
MLA	马瑞,et al."扬子克拉通西缘新生代幔源钾质-超钾质岩岩浆氧逸度及其对陆内斑岩成矿作用的启示".矿物岩石地球化学通报 (2020):794-809.

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