The main results are as follows: ( 1) The marginal parts of the plateau are dominated by thrust faulting showing compressive deformation, but the inner parts of the plateau are characterized by a series of nearly parallel and arcuated bending left lateral strike slip faults.

  • 主要内容有:1.高原边缘地带以反映压缩形变的逆断层活动为主,内部以一系列大致平行、呈弧形弯曲的左旋走滑断裂活动为主;

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