GIG OpenIR
Li, Zilong; Li, Yinqi; Chen, Hanlin; Santosh, M.; Yang, Shufeng; Xu, Yigang; Langmuir, Charles, H.; Chen, Zhongxing; Yu, Xing; Zou, Siyuan
Hf isotopic characteristics of the Tarim Permian large igneous province rocks of NW China: Implication for the magmatic source and evolution
Source PublicationJournal of Asian Earth Sciences
ISSN1367-9120
2012
Volume49Pages:191-202
Indexed BySCI
Language英语
WOS IDWOS:000303699200014
Citation statistics
Cited Times:55[WOS]   [WOS Record]     [Related Records in WOS]
Document Type期刊论文
Identifierhttp://ir.gig.ac.cn/handle/344008/18168
Collection中国科学院广州地球化学研究所
Recommended Citation
GB/T 7714
Li, Zilong,Li, Yinqi,Chen, Hanlin,et al. Hf isotopic characteristics of the Tarim Permian large igneous province rocks of NW China: Implication for the magmatic source and evolution[J]. Journal of Asian Earth Sciences,2012,49:191-202.
APA Li, Zilong.,Li, Yinqi.,Chen, Hanlin.,Santosh, M..,Yang, Shufeng.,...&Zou, Siyuan.(2012).Hf isotopic characteristics of the Tarim Permian large igneous province rocks of NW China: Implication for the magmatic source and evolution.Journal of Asian Earth Sciences,49,191-202.
MLA Li, Zilong,et al."Hf isotopic characteristics of the Tarim Permian large igneous province rocks of NW China: Implication for the magmatic source and evolution".Journal of Asian Earth Sciences 49(2012):191-202.
Files in This Item:
There are no files associated with this item.
Related Services
Recommend this item
Bookmark
Usage statistics
Export to Endnote
Google Scholar
Similar articles in Google Scholar
[Li, Zilong]'s Articles
[Li, Yinqi]'s Articles
[Chen, Hanlin]'s Articles
Baidu academic
Similar articles in Baidu academic
[Li, Zilong]'s Articles
[Li, Yinqi]'s Articles
[Chen, Hanlin]'s Articles
Bing Scholar
Similar articles in Bing Scholar
[Li, Zilong]'s Articles
[Li, Yinqi]'s Articles
[Chen, Hanlin]'s Articles
Terms of Use
No data!
Social Bookmark/Share
All comments (0)
No comment.
 

Items in the repository are protected by copyright, with all rights reserved, unless otherwise indicated.