Coexistence of Carboniferous oceanic island basalts with Permian supra‐subduction zone ophiolites in the Changning–Menglian accretionary wedge: Implication for tectonic reconstruction-Reference-Cited by-同舟云学术

Coexistence of Carboniferous oceanic island basalts with Permian supra‐subduction zone ophiolites in the Changning–Menglian accretionary wedge: Implication for tectonic reconstruction

Published:2022-11-25 Issue: Volume: Page:
ISSN:0072-1050
Container-title:Geological Journal
language:en
Short-container-title:Geological Journal

Author:

Liu Jinyu¹²,Deng Jun¹,Wang Qingfei¹,Li Gongjian¹,Li Chusi³,Ripley Edward M.³

Affiliation:

1. State Key Laboratory of Geological Processes and Mineral Resources China University of Geosciences Beijing China

2. Beijing Museum of Natural History Beijing China

3. Department of Earth and Atmospheric Sciences Indiana University Bloomington Indiana USA

Publisher

Wiley

Subject

Geology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/gj.4625

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