独山子—安集海断裂带隐伏段的探测方法综合应用研究

摘要

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.%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.