The Red River Fault Zone is a large slide and active fault zone.
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。
This paper discusses the features of neotectonic movement of Red River fault zone in two respects of geology and geomorphology.
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。
Since the Tertiary period, the Red River Fault Zone suffered both of the sinistral movement and dextral movement, but the activities of the north and the south segment were different.
断裂带自第三纪以来，经历了左旋运动、右旋运动，南北两段的活动性有一定的差异。
The range of deformation region and the magnitude of deformation show that the eastern plate of the Red River Fault zone is always the active plate for the relative movement of the fault blocks.
变形区的范围大小和变形幅度表明红河断裂的东盘地块始终是作为地块相对运动的主动盘。
The range of deformation region and the magnitude of deformation show that the eastern plate of the Red River Fault zone is always the active plate for the relative movement of the fault blocks.
变形区的范围大小和变形幅度表明红河断裂的东盘地块始终是作为地块相对运动的主动盘。
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