节点文献
独山子—安集海断裂带隐伏段的探测方法综合应用研究
APPLICATION RESEARCH ON DETECTION METHOD OF DUSHANZI-ANJIHAI FAULT’S HIDDEN SEGMENT
【摘要】 采用浅层人工地震和高密度电法两种地球物理探测手段,结合探槽剖面结果对独山子—安集海断裂位于独山子区南侧的隐伏段进行判别。分析结果表明,独山子—安集海断裂隐伏段总体走向近东西,它是由多条南倾和北倾的逆断层组成,断裂带宽度100~160 m,错断了全新世砾石层。
【Abstract】 Using shallow artificial seismic and high density resistivity methods to distinguish southern hidden segment of Dushanzi-Anjihai fault with trench profile,the results show: the southern hidden segment of Dushanzi-Anjihai fault strikes Holocene in a nearly E-W direction and was made up of several reverse faults with 100-160 meters width.
【关键词】 断裂带探测;
地球物理探测;
浅层人工地震;
高密度电法;
独山子;
【Key words】 Fault detection; Geophysical method; Shallow artificial seismic; High density resisitivity method; Dushanzi;
【Key words】 Fault detection; Geophysical method; Shallow artificial seismic; High density resisitivity method; Dushanzi;
- 【文献出处】 内陆地震 ,Inland Earthquake , 编辑部邮箱 ,2013年01期
- 【分类号】P631
- 【被引频次】5
- 【下载频次】44