Petrology and geochemistry of ultramafic rocks in the Mogok belt, Myanmar: Cumulates from high‐pressure crystallization of hydrous arc melts

Author:

Liu Tong1ORCID,Liu Chuan‐Zhou123,Chen Yi1,Guo Shun1,Sein Kyaing4,Dong Xiao‐Tao5

Affiliation:

1. State Key Laboratory of Lithospheric Evolution Institute of Geology and Geophysics, Chinese Academy of Sciences Beijing China

2. Chinese Academy of Sciences (CAS) Center for Excellence in Tibetan Plateau Earth Sciences Beijing China

3. University of Chinese Academy of Sciences Beijing China

4. Myanmar Geosciences Society, Hlaing University Campus Yangon Myanmar

5. No. 6 Institute of Geology and Mineral Resources Exploration of Shandong Province Weihai China

Funder

National Natural Science Foundation of China

National Science Fund for Distinguished Young Scholars

Publisher

Wiley

Subject

Geology

Reference55 articles.

1. Abundances of the elements: Meteoritic and solar;Anders E.;Geochimica et Cosmochimica Acta,1989

2. Jurassic to Miocene magmatism and metamorphism in the Mogok metamorphic belt and the India–Eurasia collision in Myanmar;Barley M. E.;Tectonics,2003

3. The range of spinel compositions in terresterial mafic and ultramafic rocks;Barnes S. J.;Journal of Petrology,2001

4. Cenozoic metamorphism along the Shan scarp (Myanmar): Evidences for ductile shear along the Sagaing fault or the northward migration of the eastern Himalayan syntaxis?;Bertrand G.;Geophysical Research Letters,1999

5. Magnesium isotope composition of subduction zone fluids as constrained by jadeitites from Myanmar;Chen Y.;Journal of Geophysical Research: Solid Earth,2018

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