Published November 1, 2016
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Progressive Crustal Deformation of Yinmabin Area and Its Environs, Mandalay Region
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The present paper emphasized mainly on interpretations of deformation fabrics and stress field orientation related to progressive crustal deformation and deformation patterns of the Yinmabin area and its environs during India and Asia collision in Early Cenozoic time. On the basis of microfabric as well as in addition with megastructures, there are at least five types of structural deformation, which operated within the Shan scarp fault zone and Sagaing fault zone.
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References
- Barley, M. E. et. al. (2003). Jurassic to Miocene Magmatism and Metamorphism in the Mogok Metamorphic Belt and the India Eurasia Collision in Myanmar.Tectonics, V. 22, No. 3, 10 p. Bertrand, G., Rangan, C., Maluski, H., Tin Aung Han, Myint Thein, Ohn Myint, Win Maw & San Lwin. (1999). Cenozoic Metamorphism along the Shan Scarp (Myanmar): evidence for ductile shear along the Sagaing Fault or the northward migration of the eastern Himalayan Syntaxis. Geophys. Res. Lett 26, 915 -918.