Characteristics and formation analysis of earth fissure in Anren area in Wei River Basin， China

作     者：Jianwei Qiao Zhenjiang Meng Yuyun Xia Cong Liu Quanzhong Lu Feiyong Wang Yuanqiang Zhou Haiyuan Zhao 

作者机构：China Jikan Research Institute of Engineering Investigations and Design Co.， Ltd. Shaanxi Key Laboratory for the Property and Treatment of Special Soil and Rock School of Geological Engineering and Geomatics， Chang'an University Key Laboratory of Western China Mineral Resources and Geological Engineering School of Engineering and Technology， China University of Geosciences (Beijing) 

出 版 物：《Journal of Earth Science》 (地球科学学刊(英文版))

年 卷 期：2022年

核心收录：

学科分类：081803[工学-地质工程] 08[工学] 0818[工学-地质资源与地质工程] 

基　　金：funded by the CMEC Technology Incubation Project (CMEC-KJFH-2018-02) the National Science Foundation of China (41877250) the Fundamental Research Funds for the Central Universities, CHD(300102268206 and 300102260401) Shaanxi Science and Technology Coordination Innovation Project (NO. 2011KTZB03-02-02) the National Geological Survey of China (DD20160264) 

摘      要：Since the 1950’s， 212 earth fissures have been discovered in the Wei River Basin. During a field survey in 2016， an additional 48 earth fissures were discovered in Anren area， northeast of the Wei River Basin. The characteristics and formation mechanisms of these fissures were studied through field investigations， measurements， trench excavation， and drilling. On-site investigations indicated that these earth fissures were distributed along a fault-controlled geomorphic boundary. Fissures trended at 60°–80° NE and were divided into five groups. Trenches revealed multiple secondary fissures， exposing severe soil ruptures in the shallow earth surfaces. Drilling profiles revealed that earth fissures dislocated several strata， and resembled synsedimentary faults. Seismic reflection profiles revealed buried faults beneath the earth fissures. The Anren area fissures formed in the following three stages: regional extension that initially generated multiple buried faults; seismic activity rupturing multiple strata， resulting in multiple buried fractures; and finally， erosion processes that propagated the buried fractures to the surface， forming the current earth fissures.