红河断裂带（Red River fault zone）又称哀牢山—红河构造带，为扬子地台与印支地块间的边界构造带。
本文从地质、地貌两个方面讨论了红河断裂带的新构造活动特征。
This paper discusses the features of neotectonic movement of Red River fault zone in two respects of geology and geomorphology.
红河断裂带是印藏碰撞过程中 ，印支地块被顺时针旋转挤出的走滑变形带。
The Red River Fault Zone is a large slide and active fault zone.
红河断裂带两侧古地磁结果表明，羌塘地体与扬子地台至少从早白垩世以来已连接为一个整体。
Paleomagnetic results from the both sides of Honghe fault zone have shown that the Yangzi block has been united with the Qiangtang terrane since Cretaceous.
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