Geochemical variations of anatectic melts in response to changes of P–T–H2O conditions: Implication for the relationship between dehydration and hydration melting in the Himalayan orogen-Reference-Cited by-同舟云学术

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Geochemical variations of anatectic melts in response to changes of P–T–H2O conditions: Implication for the relationship between dehydration and hydration melting in the Himalayan orogen

Published:2024-01 Issue: Volume:643 Page:121815
ISSN:0009-2541
Container-title:Chemical Geology
language:en
Short-container-title:Chemical Geology

Author:

Ji Min,Gao Xiao-Ying,Zheng Yong-Fei,Gong Bing

Funder

Fundamental Research Funds for the Central Universities

National Natural Science Foundation of China

Chinese Academy of Sciences

China Postdoctoral Science Foundation

Youth Innovation Promotion Association of the Chinese Academy of Sciences

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference123 articles.

1. Evidence for early (>44 Ma) Himalayan crustal thickening, Tethyan Himalaya, southeastern Tibet;Aikman;Earth Planet. Sci. Lett.,2008

2. Dehydration melting and Proterozoic granite petrogenesis in a collisional orogen a case from the Svecofennian of southern Finland;Andersen;J. Earth Sci.,2021

3. Granite geochemistry is not diagnostic of the role of water in the source;Bartoli;Earth Planet. Sci. Lett.,2021

4. Anatectic granites in their source region: a comparison between experiments, thermodynamic modelling and nanogranitoids;Bartoli;Lithos,2021

5. A catalytic delamination-driven model for coupled genesis of Archaean crust and sub-continental lithospheric mantle;Bédard;Geochim. Cosmochim. Acta,2006

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