Thermodynamic modeling and elemental migration for the early stage of rodingitization: An example from the Xialu massif of the Xigaze ophiolite, southern Tibet-Reference-Cited by-同舟云学术

Thermodynamic modeling and elemental migration for the early stage of rodingitization: An example from the Xialu massif of the Xigaze ophiolite, southern Tibet

Published:2021-05 Issue:3 Volume:12 Page:101125
ISSN:1674-9871
Container-title:Geoscience Frontiers
language:en
Short-container-title:Geoscience Frontiers

Author:

Duan Wen-Yong,Li Xu-Ping,Wang Ze-Li,Chen Shuang,Sun Guang-Ming,Zhao Ling-Quan

Funder

National Natural Science Foundation of China

Publisher

Elsevier BV

Subject

General Earth and Planetary Sciences

Reference101 articles.

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3. When and where did India and Asia collide?;Aitchison;J. Geophys. Res.-Solid Earth,2007

4. Structure and evolution of the Himalaya-Tibet orogenic belt;Allègre;Nature,1984

5. Rodingitization and hydration of the oceanic lithosphere as developed in the Leka ophiolite, north-Central Norway;Austrheim;Lithos,2008

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