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昌吉市庙尔沟村位于天山北麓的中低山区,地势西南高东北低,地质环境条件较差,目前调查共发现滑坡2处。通过对庙尔沟村HP1滑坡地质灾害的详细调查与测绘,对滑坡发育特征及影响因素进行深入分析,研究结果表明:HP1滑坡为新滑坡,滑动部位总体形态为平面呈不规则椭圆形,滑坡体厚度在4~18 m左右;滑动面为土岩界面,滑坡体由风积粉土、坡积砂卵砾石组成,两侧以粉土为主,中部则以砂砾石为主;地形地貌、岩土体类型、地震、降雨和人类工程是研究区滑坡形成的主要成灾因素,为后续滑坡地质灾害点的防治提供理论依据
Changji City Mier Ergou Village is located in the northern foot of the Tianshan Mountains, low topography in southwestern northeast, poor geological and environmental conditions, the survey found a total of two landslides. Based on the detailed investigation and mapping of HP1 landslide geological disasters in Miaorou Village, the landslide development characteristics and influencing factors are analyzed in depth. The results show that HP1 landslide is a new landslide. The overall shape of the landslide is irregular oval, The body thickness is about 4 ~ 18 m; the sliding surface is the earth-rock interface, the landslide body consists of aeolian silt and sloping sand and gravel, the silt is the main body on both sides and the gravel is the middle part. The topography, The types of rock and soil, earthquakes, rainfall and human engineering are the major factors that cause the landslides to form in the study area, which provides a theoretical basis for the prevention and control of the subsequent landslide geological disasters