GIG OpenIR  > 中国科学院矿物学与成矿学重点实验室  > 期刊论文
Hu, Jun; Wang, He; Wang, Min
Geochemistry and origin of the Neoproterozoic Dahongliutan banded iron formation (BIF) in the Western Kunlun orogenic belt, Xinjiang (NW China)
Source PublicationORE GEOLOGY REVIEWS
ISSN0169-1368
2017
Volume89Pages:836-857
DOI10.1016/j.oregeorev.2017.07.020
Indexed BySCI
Language英语
WOS Research AreaGeology ; Mineralogy ; Mining & Mineral Processing
WOS IDWOS:000413126900043
Citation statistics
Cited Times:4[WOS]   [WOS Record]     [Related Records in WOS]
Document Type期刊论文
Identifierhttp://ir.gig.ac.cn/handle/344008/35203
Collection中国科学院矿物学与成矿学重点实验室_期刊论文
Recommended Citation
GB/T 7714
Hu, Jun,Wang, He,Wang, Min. Geochemistry and origin of the Neoproterozoic Dahongliutan banded iron formation (BIF) in the Western Kunlun orogenic belt, Xinjiang (NW China)[J]. ORE GEOLOGY REVIEWS,2017,89:836-857.
APA Hu, Jun,Wang, He,&Wang, Min.(2017).Geochemistry and origin of the Neoproterozoic Dahongliutan banded iron formation (BIF) in the Western Kunlun orogenic belt, Xinjiang (NW China).ORE GEOLOGY REVIEWS,89,836-857.
MLA Hu, Jun,et al."Geochemistry and origin of the Neoproterozoic Dahongliutan banded iron formation (BIF) in the Western Kunlun orogenic belt, Xinjiang (NW China)".ORE GEOLOGY REVIEWS 89(2017):836-857.
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