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哀牢山(Ailaoshan)—红河剪切带是东南亚最著名的地质不连续带,多次被定为早新生代以来控制印度和亚洲会聚的重要边界。根据地层和构造对比,沿哀牢山—红河剪切带的左旋运动发生在35~17Ma,产生了一个700±200km的平错断层。普遍认为印度支那...
Ailaoshan - The Red River shear belt is the most famous geological discontinuity in Southeast Asia and has been repeatedly identified as an important border controlling the convergence of India and Asia since the early Cenozoic. According to the stratigraphic and structural comparison, the left-lateral movement along the Ailaoshan-Honghe shear zone occurred between 35 and 17 Ma, resulting in a 700 ± 200 km flat-faulted fault. It is generally accepted that Indochina ...