As a result, the Weizhou-Shigouyi detachment structure is bounded on the east and west by faults and occurs as a synclinorium comprising exotic sheeted rocks with simple deformation.

• 它在地震剖面上表现为：滑脱面以上的多层平行反射、不出现逆冲推覆前缘带复杂变形造成的杂乱反射；平面上形成与周邻明显的构造不协调性。