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川西巴塘断裂带地质灾害效应与典型滑坡发育特征
引用本文:杨志华,吴瑞安,郭长宝,张永双,兰恒星,任三绍,闫怡秋. 川西巴塘断裂带地质灾害效应与典型滑坡发育特征[J]. 中国地质, 2022, 49(2): 355-368
作者姓名:杨志华  吴瑞安  郭长宝  张永双  兰恒星  任三绍  闫怡秋
作者单位:1. 中国地质科学院地质力学研究所;2. 自然资源部活动构造与地质安全重点实验室;3. 中国地质科学院水文地质环境地质研究所;4. 中国科学院地理科学与资源研究所;5. 中国地质大学(北京)
基金项目:中国地质调查项目(DD20190319);;国家自然科学基金项目(41731287,41941019)共同资助~~;
摘    要:[研究目的]川西巴塘断裂带地质背景复杂,研究地质灾害发育特征,有利于揭示活动断裂带的地质灾害效应.[研究方法]本文在巴塘断裂带地质灾害成灾背景分析和野外调查研究的基础上,剖析了区域地质灾害分布规律与典型滑坡发育特征,探讨了巴塘断裂带的地质灾害效应.[研究结果]研究认为:(1)巴塘断裂带附近碎裂岩体结构为地质灾害孕育提供...

关 键 词:青藏高原  巴塘断裂带  地质灾害效应  地震滑坡  成灾机理  地质调查工程
收稿时间:2020-12-13
修稿时间:2021-01-03

Geo-hazard effects and typical landslide characteristics of the Batang fault zone in the western Sichuan
YANG Zhihu,WU Ruian,GUO Changbao,ZHANG Yongshuang,LAN Hengxing,REN Sanshao,YAN Yiqiu. Geo-hazard effects and typical landslide characteristics of the Batang fault zone in the western Sichuan[J]. Geology in China, 2022, 49(2): 355-368
Authors:YANG Zhihu  WU Ruian  GUO Changbao  ZHANG Yongshuang  LAN Hengxing  REN Sanshao  YAN Yiqiu
Affiliation:Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing, 100081, China;Key Laboratory of Active Tectonics and Geological safety, Ministry of Natural Resources, Beijing, 100081, China;Institute of Hydrogeology and Environmental Geology, Chinese Academy of Geological Sciences, Shijiazhuang 050061, Hebei, China;Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing, 100101, China; Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing, 100081, China;China University of Geosciences, Beijing 100083, China
Abstract:This paper is the result of the geological disaster prevention and control engineering and geological hazard prevention and control engineering.[Objective]The Batang fault zone in the western Sichuan and eastern Tibet Plateau has complex geological settings. The study on the geo-hazard development characteristics is helpful to reveal the geo-hazard effect of active fault zone.[Methods]Based on the forming background analysis and field geo-hazard investigation of the Batang fault zone, this paper analyzes the geo-hazard distribution law and typical landslide development characteristics, and discusses the geo-hazard effects of the Batang fault zone.[Results]The study shows that:(1) The fragmented rock mass structure effected by fault activity can promote the development and formation of geo-hazard, and the violent fault activity (earthquake) or the creeping activity can induce geo-hazards,and the strong geo-hazard effects mainly occur with in 3000 m on both sides of the fault. (2) Geo-hazards in the Batang fault zone have the characteristics of wide areas, uneven distribution, local concentration, and so on. There are a large number of creepy landslides and seismic landslides in the deep-cut canyon along the main stream of the Jinsha River. (3) Seismic landslides and ancient landslides are developed in the Batang fault zone, and some landslides directly cross the fault zone. The superimposed influence of internal and external forces such as faults, rainfall and human engineering, has induced some local revival of some landslides.[Conclusions] The Batang fault has a significant control effect on regional geo-hazard development and distribution.Some residential areas and roads in the Batang fault zone are at geo-hazard risk. The town planning area should be far away from the river valley bank slopes and debris flow accumulation fans and other areas vulnerable to geo-hazard. The research results have important scientific significance for understanding the geo-hazard effects of the active fault zone in the eastern Tibet Plateau and for disaster prevention and mitigation.Highlights: The geo-hazard effect and disaster mechanism of the Batang active fault zone in the eastern Tibet are deeply analyzed.
Keywords:eastern Tibet Plateau  Batang fault zone  geo-hazard effects  seismic landslides  disaster mechanism  geological survey engineering
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