A review of geological characteristics and time–space distribution of cobalt deposits in the Central Asian Orogenic Belt, Xinjiang, Northwest China-Reference-Cited by-同舟云学术

A review of geological characteristics and time–space distribution of cobalt deposits in the Central Asian Orogenic Belt, Xinjiang, Northwest China

Published:2022-06-11 Issue:8 Volume:65 Page:1388-1408
ISSN:0020-6814
Container-title:International Geology Review
language:en
Short-container-title:International Geology Review

Author:

Yang Fuquan¹,Liu Guoren²,Zhang Hanqing³,Yang Chengdong³,Li XiaoZhuang¹,Li Qiang¹,Li Ning⁴,Zhang Zhenlong¹

Affiliation:

1. Key Laboratory of Metallogeny and Mineral Assessment, Ministry of Natural Resources, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing, China

2. Xinjiang Research Center for Mineral Resources, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi, Xinjiang, China

3. No. 4 Geological Party of the Xinjiang Bureau of Geo-Exploration & Mineral Development, Altay, Xinjiang, China

4. College of Mining Engineering, Taiyuan University of Technology, Taiyuan, Shanxi, China

Funder

‘Introducing Talents to Western China’ of the Chinese Academy of Sciences (“Introducing Talents to Western China” of the Chinese Academy of Sciences

National Natural Science Foundation of China Program

“Introducing Talents to Western China” of the Chinese Academy of Sciences

Publisher

Informa UK Limited

Subject

Geology

Link

https://www.tandfonline.com/doi/pdf/10.1080/00206814.2022.2087111

Reference133 articles.

1. Ao, S.J, 2010, Paleozoic accretionary tectonics of the Beishan Orogen: Insights from anatomy of ophiolites and Alaskan-type complexes: Unpublished PhD. thesis (in Chinese with English abstract). Institute of Geology and Geophysics, Chinese Academy of Sciences.

2. Source characteristics and tectonic setting of mafic–ultramafic intrusions in North Xinjiang, NW China: Insights from the petrology and geochemistry of the Lubei mafic–ultramafic intrusion

3. Formation of the Lubei magmatic Ni–Cu deposit in a post-subduction setting in East Tianshan, North West China

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