The triggering mechanism for the salt mud tectonics was gravitational gliding accompanying regional extension.

重力滑动作用表现为触发盐-泥层的聚集-隆升和引起薄皮滑脱作用.

互联网

Salt mud bed accumulation and upwelling and thin - skinned detachment led to gravitational gliding.

由此文中将盐-泥构造演化历程划分为盐-泥枕发育期和滑脱断层-盐-泥滚 - 盐-泥核背斜发育期.

互联网