８０年代以来，广西小平阳岩溶区出现了大量的地裂缝。通过调查研究．这些地裂缝的形成是受多种因素控制的．其中包括构造、土体性质、水的作用、地形地貌、气候及植被等因素。在上述因素中．构造是主导因素，上体性质是基础因素．其它则为诱发因素，也是因地质环境要素变化所引起的因素。主导因素是通过诱发因素起作用的．并最终通过土体性质因素导致产土地裂缝。 Since the 1980s, there have been a large number of ground fissures in the Xiaopingyang karst area of ​​Guangxi. Through the investigation. The formation of these ground fissures is controlled by many factors. Including the structure, soil properties, the role of water, topography, climate and vegetation and other factors. Among the above factors. Structure is the dominant factor, the upper body is the basic factor. Others are induced factors, but also due to changes in the geological environment factors caused. The dominant factor is through the trigger factor. And ultimately lead to cracks in the land through the nature of the soil.