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根据滑坡区地形地貌特征、岩体结构特征以及滑坡群的工程地质特征分析认为 ,尽管滑坡群中的 5个滑坡共同发育在一个大型圈谷地貌中 ,但它们并非是一次下滑所形成 ,而是具有一定的时序性
According to the topography of the landslide area, the structural characteristics of the rock mass and the engineering geological characteristics of the landslide group, it is considered that although the five landslides in the landslide group co-develop in a large valley and valley landscape, they are not formed by a single decline but rather Has a certain timing