疏勒河断裂中段VLF响应特点及地质解释  

VLF CHARACTER AND ITS GEOLOGICAL INTERPRETATION IN THE MIDDLE REGION OF SHULE RIVER FAULT ZONE

作　　者：莫撼[1] 熊章强[1] 

机构地区：[1]华东地质学院地球科学系

出　　处：《华东地质学院学报》1995年第3期249-251,共3页Journal of East China Geological Institute

摘　　要：疏勒河断裂带中段为一隐伏基底断裂。由于规模较大，并且充填了低阻的构造角砾岩，因此对ＶＬＦ有很好的响应。本文分析了该构造的ＶＬＦ响应特点，指出在本区用ＶＬＦ方法寻找隐伏构造的有效性和局限性。The middle region of Shule River Fault Zone is a blind basement fault zone.TheVLF response is very good becausc of its large scale and being filled with the structural breccia oflow resistivity.The VLF character for the fault zone was discussed.It is pointed that the effec-tiveness and limitation of searching blind fault with VLF method.

关 键 词：疏勒河 断裂 甚低频 电磁法 地质解释 VLF响应 

分 类 号：P542.3[天文地球—构造地质学]