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独山子—安集海断裂带隐伏段的探测方法综合应用研究
引用本文:葛鸣,赵纯青,马新龙.独山子—安集海断裂带隐伏段的探测方法综合应用研究[J].内陆地震,2013,27(1):38-44.
作者姓名:葛鸣  赵纯青  马新龙
作者单位:1. 新疆维吾尔自治区地震局,新疆乌鲁木齐,830011
2. 新疆昌吉方汇水电设计有限公司,新疆昌吉,831100
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100~160m,错断了全新世砾石层。

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

APPLICATION RESEARCH ON DETECTION METHOD OF DUSHANZI-ANJIHAI FAULTS HIDDEN SEGMENT
GE Ming , ZHAO Chun-qing , MA Xin-long.APPLICATION RESEARCH ON DETECTION METHOD OF DUSHANZI-ANJIHAI FAULTS HIDDEN SEGMENT[J].Inland Earthquake,2013,27(1):38-44.
Authors:GE Ming  ZHAO Chun-qing  MA Xin-long
Institution:1.Earthquake Administration of Xinjiang Uygur Autonomous Region,Urumqi 830011,Xinjiang,China; 2.The Huifang Hydroelectric Engineering Limited Company,Changji 831100,Xinjiang,China)
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.
Keywords:Fault detection  Geophysical method  Shallow artificial seismic  High density resisitivity method  Dushanzi
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