Role and origin of water-fluxed melting in the generation of High Himalayan leucogranites
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Published:2024-05
Issue:
Volume:266
Page:106118
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ISSN:1367-9120
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Container-title:Journal of Asian Earth Sciences
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language:en
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Short-container-title:Journal of Asian Earth Sciences
Author:
Lei KaiORCID,
Wang Xuan-CeORCID,
Wilde Simon A.
Reference90 articles.
1. Age and thermal history of Eo- and Neohimalayan granitoids, eastern himalaya;Aikman;J. Asian Earth Sci.,2012
2. The origin of eo- and neo-himalayan granitoids, eastern Tibet;Aikman;J. Asian Earth Sci.,2012
3. Thermometers and thermobarometers in granitic systems;Anderson;Rev. Mineral. Geochem.,2008
4. REE fractionation and Nd-isotope disequilibrium during crustal anatexis: constraints from Himalayan leucogranites;Ayres;Chem. Geol.,1997
5. Barker, F., 1979. Chapter 1 - Trondhjemite: Definition, Environment and Hypotheses of Origin, in: Barker, F. (Ed.), Developments in Petrology, Trondhjemites, Dacites, and Related Rocks. Elsevier, pp. 1–12. doi: 10.1016/B978-0-444-41765-7.50006-X.