Os isotopic evidence for a carbonaceous chondritic mantle source for the Nagqu ophiolite from Tibet and its implications

	Os isotopic evidence for a carbonaceous chondritic mantle source for the Nagqu ophiolite from Tibet and its implications
	Huang, QS (Huang QiShuai) ; Shi, RD (Shi RenDeng) ; Liu, DL (Liu DeLiang) ; Zhang, XR (Zhang XiaoRan) ; Fan, SQ (Fan ShuaiQuan) ; Ding, L (Ding Lin)
刊名	CHINESE SCIENCE BULLETIN
	2013
卷号	58 期号:1 页码:92-98
通讯作者	Huang, QS (通讯作者),Chinese Acad Sci, Inst Tibetan Plateau Res, Key Lab Continental Collis & Plateau Uplift, Beijing 100101, Peoples R China.
合作状况	国内
学科主题	地质学
收录类别	SCI
语种	英语
WOS记录号	WOS:000313736600015
公开日期	2014-06-11
内容类型	期刊论文
源URL	[http://ir.itpcas.ac.cn/handle/131C11/2816]
专题	青藏高原研究所_图书馆
推荐引用方式 GB/T 7714	Huang, QS ,Shi, RD ,Liu, DL ,et al. Os isotopic evidence for a carbonaceous chondritic mantle source for the Nagqu ophiolite from Tibet and its implications[J]. CHINESE SCIENCE BULLETIN,2013,58(1):92-98.
APA	Huang, QS ,Shi, RD ,Liu, DL ,Zhang, XR ,Fan, SQ ,&Ding, L .(2013).Os isotopic evidence for a carbonaceous chondritic mantle source for the Nagqu ophiolite from Tibet and its implications.CHINESE SCIENCE BULLETIN,58(1),92-98.
MLA	Huang, QS ,et al."Os isotopic evidence for a carbonaceous chondritic mantle source for the Nagqu ophiolite from Tibet and its implications".CHINESE SCIENCE BULLETIN 58.1(2013):92-98.