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疏勒河断裂中段VLF响应特点及地质解释
引用本文:莫撼 熊章强. 疏勒河断裂中段VLF响应特点及地质解释[J]. 华东地质学院学报, 1995, 18(3): 249-251
作者姓名:莫撼 熊章强
作者单位:华东地质学院地球科学系
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。

关 键 词:疏勒河 断裂 甚低频 电磁法 地质解释 VLF响应

VLF CHARACTER AND ITS GEOLOGICAL INTERPRETATION IN THE MIDDLE REGION OF SHULE RIVER FAULT ZONE
Mo Han Xiong Zhangqiang. VLF CHARACTER AND ITS GEOLOGICAL INTERPRETATION IN THE MIDDLE REGION OF SHULE RIVER FAULT ZONE[J]. Journal of East China Institute of Technology, 1995, 18(3): 249-251
Authors:Mo Han Xiong Zhangqiang
Abstract:
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.
Keywords:Shule river  fault zone  very low frequency  electramagnetic method  response
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