中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Os isotopic evidence for a carbonaceous chondritic mantle source for the Nagqu ophiolite from Tibet and its implications

文献类型:期刊论文

作者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
出版日期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
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.

入库方式: OAI收割

来源:青藏高原研究所

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