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| POSITION AND CHARACTERISTICS OF SIGNIFICANT FAULTS IN MYANMAR |
| ZHOU Xi-lin1, LI Xin-ren1, YAN Cheng-min2, WANG Chang-bing1, ZHU Lin1 |
1. No.209 Geological Party, Yunnan Bureau of Geology for Nuclear Industry, Kunming 650031, China;
2. Regional Geological Survey Party, Yunnan Bureau of Geology and Mineral Resources, Yuxi 653100, Yunnan Province, China |
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Abstract With field survey and processing of previous data, nine faults are identified as the tectonic boundaries in Myanmar, which are:Naga Yoma-Rakhine Yoma thrust fault (F1), Pinlebu-Pye extensional fault (F2), Sagaing-Bago dextral strike-slip fault (F3), Putao-Kadu thrust fault (F4), Ringhkung-Phamo extensional fault (F5), Namhkam-Mogok dextral strike-slip fault (F6), Mandalay-Bago sinistral strike-slip fault (F7), Xidang-Santa sinistral strike-slip fault (F8) and Mong Ping-Chiang Mai thrust fault (F9)
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Received: 16 May 2016
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2017, Vol. 26 
