Subduction and retreat of Permian oceanic plates in the East Kunlun Orogenic Belt: evidence from mafic-ultramafic intrusive rocks-Reference-Cited by-同舟云学术

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Subduction and retreat of Permian oceanic plates in the East Kunlun Orogenic Belt: evidence from mafic-ultramafic intrusive rocks

Published:2024-01-02 Issue:15 Volume:66 Page:2717-2740
ISSN:0020-6814
Container-title:International Geology Review
language:en
Short-container-title:International Geology Review

Author:

Hu Chaobin¹²,Feng Chengyou³,Li Meng²,Zha Xianfeng²,Gao Xiaofeng²,Gao Zikun¹,Li Ming¹

Affiliation:

1. Faculty of Engineering, Lishui University, Lishui, China

2. Xi’an Center of Geological Survey, CGS, Orogen Research Center of China Geological Survey, Xi’an, China

3. Institute of Exploration Technology, Chinese Academy of Geological Sciences, Langfang, China

Funder

China Geological Survey projects

national natural science foundation of China

Publisher

Informa UK Limited

Link

https://www.tandfonline.com/doi/pdf/10.1080/00206814.2023.2297417

Reference142 articles.

1. Petrology of the Motaghairat mafic–ultramafic complex, Eastern Desert, Egypt: A high-Mg post-collisional extension-related layered intrusion

2. Correction of common lead in U–Pb analyses that do not report 204Pb

3. Geochronology and geochemistry of Early Permian mafic–ultramafic complexes in the Beishan area, Xinjiang, NW China: Implications for late Paleozoic tectonic evolution of the southern Altaids

4. Basal continental mantle lithosphere displaced by flat-slab subduction

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