Carboniferous back-arc bimodal rocks in West Kunlun during northward subduction of the Paleo-Tethys-Reference-Cited by-同舟云学术

Carboniferous back-arc bimodal rocks in West Kunlun during northward subduction of the Paleo-Tethys

Published:2023-07-06 Issue: Volume: Page:1-19
ISSN:0020-6814
Container-title:International Geology Review
language:en
Short-container-title:International Geology Review

Author:

Xia Ying¹,Sui Qinglin²³,He Yongkang⁴,Ji Wenhua⁴,Chen Denghui⁴,Zhao Xiaojian⁴,Zhao Min⁴,Gao Xiaofeng⁴,Wang Kun³,Zhang Lipeng³,He Haiyang²,Wang Jinfeng²,Chen Yue¹

Affiliation:

1. College of Earth Sciences, Chengdu University of Technology, Chengdu, China

2. School of Resource Environment and Safety Engineering, University of South China, Hengyang, China

3. Center of Deep Sea Research, Institute of Oceanology, Chinese Academy of Sciences, Qingdao, China

4. Xi’an Center of Geological Survey, Centre for Orogenic Belt Geology, China Geological Survey, Xi’an, China

Funder

National Natural Science Foundation of China

the Second Tibetan Plateau Scientific Expedition and Research

Natural Science Basic Research Program of Shaanxi

the Provincial Key R&D Program of Xinjiang Autonomous Region

Research Foundation of Education Bureau of Hunan Province

Publisher

Informa UK Limited

Subject

Geology

Link

https://www.tandfonline.com/doi/pdf/10.1080/00206814.2023.2233016

Reference110 articles.

1. Laser Ablation ICPMS study of trace element partitioning between plagioclase and basaltic melts: an experimental approach

2. Effects of repetitive emplacement of basaltic intrusions on thermal evolution and melt generation in the crust

3. Igneous zircon: trace element composition as an indicator of source rock type

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