• 中国科技核心期刊
  • 中国科技论文统计源期刊
LI Xin-ren, ZHOU Xi-lin, YAN Cheng-min, WANG Chang-bing, LI Yu-bing. DIVISION AND CHARACTERISTICS OF THE GEOTECTONIC UNITS OF MYANMAR[J]. Geology and Resources, 2017, 26(1): 99-104. DOI: 10.13686/j.cnki.dzyzy.2017.01.018
Citation: LI Xin-ren, ZHOU Xi-lin, YAN Cheng-min, WANG Chang-bing, LI Yu-bing. DIVISION AND CHARACTERISTICS OF THE GEOTECTONIC UNITS OF MYANMAR[J]. Geology and Resources, 2017, 26(1): 99-104. DOI: 10.13686/j.cnki.dzyzy.2017.01.018

DIVISION AND CHARACTERISTICS OF THE GEOTECTONIC UNITS OF MYANMAR

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  • Received Date: May 08, 2016
  • Revised Date: June 07, 2016
  • Available Online: December 29, 2022
  • Published Date: February 27, 2017
  • On the basis of field survey, with collected previous data, the authors divide the geotectonics of Myanmar into 5 first-ordered tectonic units, including 10 second-ordered tectonic units. They are, from west to east, 1) West Kachin-Pakhine suture zone (E-N1) (Ⅰ), with Chin-Pakhine suture zone (E-N1) (Ⅰ1) and West Kachin suture zone (E-N1) (Ⅰ2);2) West Myanmar-Pulau Sumatera arc basin system (E-N1) (Ⅱ), with Monywa-Pathein island arc belt (E-N1) (Ⅱ1), Shwebo-Yangon back-arc basin (E-N,) (Ⅱ2) and Myitkyina back-arc basin (E-N1) (Ⅱ3);3) Tengshong-Kra Peninsula orogenic belt (T3-K) (Ⅲ), with Bhamo continental marginal arc (T3-K) (Ⅲ1), Mawiamyine continental marginal arc (T3-K) (Ⅲ2) and Tanintharyi block (Pz2) (Ⅲ3);4) Baoshan-Shanbang landmass (€-T2) (Ⅳ);and 5) Changning-Menglian-Chiang Let suture zone (C-T2) (Ⅴ). The tectonic units are bounded by 9 faults, which, from west to east, are:Naga Yoma-Rakhine Yoma thrust fault (F1), Pinlebu-Pye extensional faults (F2), Sagaing-Bago dextral strike-slip fault (F3), Putao-Kadu thrust fault (F4), Ringhkung-Phamo extensional faults (F5), Namhkam-Mogok dextral strike-slip fracture (F6), Mandalay-Bago sinistral strike-slip fracture (F7), Xidang-santa sinistral strike-slip fracture (F8) and Mong Ping-Chiang Mai thrust fault (F9).
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