Continuous disproportionate growth of Gubei fault formed the palaeogeomorphology of Gubei slope belt with groove alternating with roof and with abrupt and gentle change.
孤北断层持续不均衡发育形成孤北斜坡带沟梁相间、陡缓变化的古地貌，古地貌控制了隐蔽圈闭的平面分布。
Abrupt slope structure belt was one of the important structure units for asymmetric fault basin.
陡坡构造带是不对称断陷盆地重要的构造单元。
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