GIG OpenIR
Wang, Changle; Zhang, Lianchang; Lan, Caiyun; Dai, Yanpei
Petrology and geochemistry of the Wangjiazhuang banded iron formation and associated supracrustal rocks from the Wutai greenstone belt in the North China Craton: Implications for their origin and tectonic setting
Source PublicationPrecambrian Research
ISSN0301-9268
2014
Volume255Pages:603-626
Indexed BySCI
Language英语
Document Type期刊论文
Identifierhttp://ir.gig.ac.cn/handle/344008/29352
Collection中国科学院广州地球化学研究所
Recommended Citation
GB/T 7714
Wang, Changle,Zhang, Lianchang,Lan, Caiyun,et al. Petrology and geochemistry of the Wangjiazhuang banded iron formation and associated supracrustal rocks from the Wutai greenstone belt in the North China Craton: Implications for their origin and tectonic setting[J]. Precambrian Research,2014,255:603-626.
APA Wang, Changle,Zhang, Lianchang,Lan, Caiyun,&Dai, Yanpei.(2014).Petrology and geochemistry of the Wangjiazhuang banded iron formation and associated supracrustal rocks from the Wutai greenstone belt in the North China Craton: Implications for their origin and tectonic setting.Precambrian Research,255,603-626.
MLA Wang, Changle,et al."Petrology and geochemistry of the Wangjiazhuang banded iron formation and associated supracrustal rocks from the Wutai greenstone belt in the North China Craton: Implications for their origin and tectonic setting".Precambrian Research 255(2014):603-626.
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
[Wang, Changle]'s Articles
[Zhang, Lianchang]'s Articles
[Lan, Caiyun]'s Articles
Baidu academic
Similar articles in Baidu academic
[Wang, Changle]'s Articles
[Zhang, Lianchang]'s Articles
[Lan, Caiyun]'s Articles
Bing Scholar
Similar articles in Bing Scholar
[Wang, Changle]'s Articles
[Zhang, Lianchang]'s Articles
[Lan, Caiyun]'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.