Scheelite and coexisting F-rich zoned garnet, vesuvianite, fluorite, and apatite in calc-silicate rocks from the Mogok metamorphic belt, Myanmar: Implications for metasomatism in marble and the role of halogens in W mobilization and mineralization-Reference-Cited by-同舟云学术

Scheelite and coexisting F-rich zoned garnet, vesuvianite, fluorite, and apatite in calc-silicate rocks from the Mogok metamorphic belt, Myanmar: Implications for metasomatism in marble and the role of halogens in W mobilization and mineralization

Published:2016-03 Issue: Volume:117 Page:82-106
ISSN:1367-9120
Container-title:Journal of Asian Earth Sciences
language:en
Short-container-title:Journal of Asian Earth Sciences

Author:

Guo Shun,Chen Yi,Liu Chuan-Zhou,Wang Jian-Gang,Su Bin,Gao Yi-Jie,Wu Fu-Yuan,Sein Kyaing,Yang Yue-Heng,Mao Qian

Funder

Chinese Academy of Sciences

National Basic Research Program of China

National Science Foundation of China

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geology

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3. The role of fluorine in the concentration and transport of lithophile trace elements in felsic magmas: insights from the Gawler Range Volcanics, South Australia;Agangi;Chem. Geol.,2010

4. Carbon dioxide released from subduction zones by fluid-mediated reactions;Ague;Nat. Geosci.,2014

5. Assessing metasomatic mass and volume changes using the bootstrap, with application to deep crustal hydrothermal alteration of marble;Ague;Econ. Geol.,1996

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