Carboniferous variation of crustal thickness and subduction angles in Eastern Tianshan, NW China: evidence from the petrogenesis of the magmatic rocks in the Aqishan

Carboniferous variation of crustal thickness and subduction angles in Eastern Tianshan, NW China: evidence from the petrogenesis of the magmatic rocks in the Aqishan–Yamansu Belt

Published:2022-04-06 Issue:5 Volume:65 Page:682-705
ISSN:0020-6814
Container-title:International Geology Review
language:en
Short-container-title:International Geology Review

Author:

Wu Bin¹,Long Xiaoping¹,Zhang Shitao¹,Zhang Yunying²,Huang Zongying³,Du Long⁴

Affiliation:

1. State Key Laboratory of Continental Dynamics, Department of Geology, Northwest University, 710069 Xi’an, China

2. Key Laboratory of Ocean and Marginal Sea Geology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, 510301, Guangzhou China

3. State Key Laboratory of Isotope Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou, China

4. Shandong Provincial Key Laboratory of Depositional Mineralization & Sedimentary Minerals, Shandong University of Science and Technology, 266590, Qingdao, China

Funder

National Natural Science Foundation of China

National Key Research and Development Project

Publisher

Informa UK Limited

Subject

Geology

Link

https://www.tandfonline.com/doi/pdf/10.1080/00206814.2022.2059710

Reference145 articles.

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4. BGMRXUAR (Bureau of Geology and Mineral Resources of Xinjiang Uygur Autonomous Region) 1993, Regional geology of Xinjiang Uygur autonomous region, Beijing: Geological Publishing House in Chinese, p. 1–841.

5. A-type granites and related rocks: Evolution of a concept, problems and prospects

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