桂西巴马地区极高Ti/Y值基性岩地球化学特征——来自峨眉山地幔柱高Ti母岩浆?

GIG OpenIR

	黄文龙; 刘希军; 时毓; 许继峰; 廖帅; 郭琳; 吴伟男; 李政林; 梁琼丹
	桂西巴马地区极高Ti/Y值基性岩地球化学特征——来自峨眉山地幔柱高Ti母岩浆?
Source Publication	地质通报
ISSN	1671-2552
	2015
Volume	34 Issue:2-3 Pages:474-486
Language	中文
CSCD ID	CSCD:5392146
Indexed By	CSCD
Citation statistics	Cited Times:6[CSCD] [CSCD Record]
Document Type	期刊论文
Identifier	http://ir.gig.ac.cn/handle/344008/31382
Collection	中国科学院广州地球化学研究所
Recommended Citation GB/T 7714	黄文龙,刘希军,时毓,等. 桂西巴马地区极高Ti/Y值基性岩地球化学特征——来自峨眉山地幔柱高Ti母岩浆?[J]. 地质通报,2015,34(2-3):474-486.
APA	黄文龙.,刘希军.,时毓.,许继峰.,廖帅.,...&梁琼丹.(2015).桂西巴马地区极高Ti/Y值基性岩地球化学特征——来自峨眉山地幔柱高Ti母岩浆?.地质通报,34(2-3),474-486.
MLA	黄文龙,et al."桂西巴马地区极高Ti/Y值基性岩地球化学特征——来自峨眉山地幔柱高Ti母岩浆?".地质通报 34.2-3(2015):474-486.

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