Water-fluxed melting and rheological weakening within the continental-scale Ailaoshan-Red River strike-slip shear zone, Western Yunnan, China-Reference-Cited by-同舟云学术

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Water-fluxed melting and rheological weakening within the continental-scale Ailaoshan-Red River strike-slip shear zone, Western Yunnan, China

Published:2025-08 Issue: Volume:197 Page:105416
ISSN:0191-8141
Container-title:Journal of Structural Geology
language:en
Short-container-title:Journal of Structural Geology

Author:

Tao Lirong^ORCID,Cao Shuyun^ORCID,Li Wenyuan,Cheng Xuemei,Liu Jianhua,Dong Yanlong^ORCID,Wang Haobo,zhan Lefan,Zhou Dingkui,Fan Jianwei,Tian Yun

Funder

National Natural Science Foundation of China

Publisher

Elsevier BV

Reference130 articles.

1. The origin of eo- and neo-himalayan granitoids, eastern Tibet;Aikman;J. Asian Earth Sci.,2012

2. Dehydration melting and the relationship between granites and granulites;Aranovich;Precambr. Res.,2014

3. Crustal channel flows: 1. Numerical models with applications to the tectonics of the Himalayan‐Tibetan orogen;Beaumont;J. Geophys. Res. Solid Earth,2004

4. Tectonically controlled fluid flow and water-assisted melting in the middle crust: an example from the Central Alps;Berger;Lithos,2008

5. Himalayan leucogranites: a review of geochemical and isotopic characteristics, timing of formation, genesis, and rare metal mineralization;Cao;Earth Sci. Rev.,2022

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