缅甸重要断裂的位置与特征

    POSITION AND CHARACTERISTICS OF SIGNIFICANT FAULTS IN MYANMAR

    • 摘要: 为了解周边国家的地质构造特征,经实地调研与前人资料整理,将缅甸构造单元边界确认为9条断裂.即:那加山-若开山逆冲断裂(F1)、平梨铺-卑谬伸展断裂(F2)、实皆-勃固右行平移断裂(F3)、葡萄-格杜逆冲断裂(F4)、英昆-八莫伸展断裂(F5)、南坎-抹谷右行平移断裂(F6)、曼德勒-垒固左行平移断裂(F7)、锡当-三塔左行平移断裂(F8)、孟宾-清迈逆冲断裂(F9).这9条断裂构成钦邦-若开邦结合带(E-N1)(Ⅰ1)、西克钦邦结合带(E-N1)(Ⅰ2)、蒙育瓦-勃生岛弧带(E-N1)(Ⅱ1)、瑞保-仰光弧后盆地(E-N1)(Ⅱ2)、密支那岛弧带(E-N1)(Ⅱ3)、八莫陆缘弧(T3-K)(Ⅲ1)、毛淡棉陆缘弧(T3-K)(Ⅲ2)、德林依达地块(Pz2)(Ⅲ3)、保山-掸邦陆块(C-T2)(Ⅳ)、昌宁-孟连-清莱结合带(C-T2)(Ⅴ)10个一级、二级大地构造单元的边界.

       

      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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