The north east fracture which is the south boundary of Yanshan faultblock shows relative notable sinistral movement.
燕山断块南边界的北东向断裂存在着较显著的左旋运动。
2
In fact, the movement of the faultblock in the deformation field controls the alternate slips of intersecting faults.
交叉断层的交替活动实际上由变形场中块体的运动所控制。
3
In the piedmont zone of fault-block mountains the pediments and tectonic terraces developed during the same tectonic movement are possessed of a certain paragenetic relation.