Metamorphic, deformation, fluids and geological significance of low-temperature retrograde mylonites of Diancangshan metamorphic massif along Ailaoshan-Red River strike-slip fault zone, Yunnan, China

Author:

Cheng Xuemei,Cao Shuyun,Li Junyu,Yu Zunpu,Dong Yanlong,Lv Meixia,Liu Junlai

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences

Reference57 articles.

1. Burchfiel B C, Wang E. 2003. Northwest-trending, middle Cenozoic, leftlateral faults in southern Yunnan, China, and their tectonic significance. J Struct Geol, 25: 781–792

2. Barr S M, Macdonald A S, Miller B V, Reynolds P H, Rhodes B P, Yokart B. 2002. New U-Pb and 40Ar/39Ar ages from the Doi Inthanon and Doi Suthep metamorphic core complexes, northwestern Thailand. Bangkok: Symposium on Geology of Thailand. 284–294

3. Bertrand G, Rangin C. 2003. Tectonics of the western margin of the Shan plateau (central Myanmar): implication for the India–Indochina oblique convergence since the Oligocene. J Asian Earth Sci, 21: 1139–1157

4. Cao S Y, Liu J L. 2006. Modern techniques for the analysis of rock microstructure: EBSD and its application (in Chinese). Adv Earth Sci, 21: 1091–1096

5. Cao S Y. 2007. Microstructures and deformation mechanisms of high temperature mylonites in Diancangshan, Western Yunnan (in Chinese). Master Dissertation. Beijing: China University of Geosciences. 1–113

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