节点文献

2011年10月16日新疆精河县5.0级地震震害特征及发震构造

THE CHARACTERISTIC OF SEIMIC HAZARD AND SEISMOGENIC STRUCTURE OF JINGHE EARTHQUAKE WITH MS5.0 XINJIANG ON OCT 16TH,2011

  • 推荐 CAJ下载
  • PDF下载
  • 不支持迅雷等下载工具,请取消加速工具后下载。

【作者】 陈建波谭明吴国栋胡伟华孙甲宁唐丽华张振斌

【Author】 CHEN Jian-bo,TAN Ming,WU Guo-dong,HU Wei-hua,SUN Jia-ning,ZHANG Zhen-bin(Earthquake Administration of Xinjiang Uygur Autonomous Region,Urumqi 830011,Xinjiang,China)

【机构】 新疆维吾尔自治区地震局

【摘要】 通过对新疆精河5.0级地震现场调查,分析了灾区局部场地效应及房屋震害特征,对震害特点进行了较为全面的分析总结。震害调查显示,灾区房屋主要以老旧的土坯房为主,地震作用使本身老旧的房屋裂缝加宽,破坏加重。同时,受局部场地差异影响,灾区房屋震害具有明显的南北分带的特点。另外,根据地震现场考察,此次地震的发震构造为库松木楔克山前断层,该断裂是发育在北天山山前逆冲推覆体前缘的一条全新世活动断层,沿断裂断错晚更新世以来的各级地貌面和沟谷阶地,并在地表形成断层陡坎和古地震地表变形遗迹。

【Abstract】 According to earthquake site investigation of Jinghe earthquake with MS 5.0,the authors analyze site effects and characteristics of earthquake hazards in earthquake-striken area and summarizes features of earthquake damage.It has been showed that: most buildings in the earthquake-striken area were adobe building;they were severe damaged by earthquake;the damage building showed south-north zonation;the seismogonic structure was Kusongmuqike piedmont fault which was a Holocene active fault and dislocated the valley of Late Palaeozoic stratum,formed fault scarp and surface deformation on the ground.

【基金】 新疆地震科学基金项目(201112)资助
  • 【分类号】P315.9
  • 【被引频次】1
  • 【下载频次】68
节点文献中: 

本文链接的文献网络图示:

本文的引文网络