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Title:: Characteristics and Developmental Laws of Geological Hazards along G318 Lhasa-Shigatse

作者:: 扶敏¹; 2; 詹涛¹; 2; 许冲³; 谢超⁴; (1.重庆市地质矿产勘查开发局107地质队,重庆 401120; 2.重庆江北地质工程勘察院,重庆 401120; 3.中国地震局地质研究所活动构造与火山重点实验室,北京 100029; 4.中国地震局第二监测中心,陕西西安 710054)

Author(s):: FU Min¹; 2; ZHAN Tao¹; 2; XU Chong³; XIE Chao⁴; (1. 107 Geological Team,Chongqing Bureau of Geology and Minerals Exploration,Chongqing 401120,China)(2. Chongqing Jiangbei Institute of Geo-Engineering Investigation,Chongqing 401120,China)(3. Key Laboratory of Active Tectonics and Volcano,Institute of Geology,China Earthquake Administration,Beijing 100029,China)(4. The Second Monitoring and Application Center,China Earthquake Administration,Xi'an 710054,Shaanxi,China)

摘要:: 利用高分辨率遥感影像目视解译技术,结合野外调查,对318国道拉萨—日喀则段沿线两侧10 km范围内的崩塌、滑坡与泥石流地质灾害开展解译与调查,并分析其特点与发育规律。结合研究区高程、坡度、坡向与地层分布,统计了崩塌与滑坡的空间分布规律。结果表明:研究区内发育有79处崩塌、117处滑坡与133条泥石流沟。面积为0.01～0.1 km²的崩塌有45处,崩塌高度主要在300 m以内,300～700 m崩塌体数量随高度增加而减少; 面积为0.1～0.01 km²滑坡有74处,包括一处面积大于10 km²的巨型滑坡体,滑坡的高度主要集中在100～300 m,包括54处滑坡体; 面积在1～10 km²和10～100 km²的泥石流沟分别为70条和39条。崩塌多发生在4.0～4.5 km高程、20°～30°坡度、南坡向、白垩纪(K)地层中,滑坡多发生在4.0～4.5 km高程、20°～30°坡度、NE坡向、三叠纪(T)地层中。

Abstract:: Combine high-resolution remote sensing image visual interpretation technology with field investigation,we carried out detailed interpretation and investigation of collapse,landslide and debris flow within 10 km on both sides along G318 Lhasa-Shigatse and analyzed their characteristics and developmental regularities. Then we calculated the spatial distribution regularities of collapse and landslide according to the elevation,slope,aspect and stratum distribution of the study area. The result showed that there are 329 places of disasters categories,among which there are 79 collapses,117 landslides,and 133 debris flows. There are 45 collapses with area in the range of 0.1～0.01 km²,and the height of collapses is mainly within 300 m,while the collapses in the height of 300～700 m tends to decrease with height; 74 landslides with area in the range of 0.1～0.01 km² developed,including a giant landslide with an area larger than 10 km²,and there are 54 landslides in the height within 100～300 m.There are 70 and 39 debris flows with area in the range of 1～10 km² and 10～100 km²,respectively. Collapses mostly occur in the strata with the elevation of 4.0～4.5 km,the slope of 20°～30°,south slope direction and Cretaceous(K). Landslides mostly occur in the strata with the elevation of 4.0～4.5 km,the slope of 20°～30°,NE slope direction and Triassic(T).