用地球物理数据描述地震危险区和断层

M. Mekkawi, El Sayed A Fergani, Klaled A Abdella
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引用次数: 3

摘要

了解和成像西南开罗带的真实地震构造对于消除这个危险地震带的风险至关重要,该地震带被埃及人口密度最高的省份包围。本研究利用研究区最新地震目录资料和航磁资料,追踪引起地震活动的地下活动断层。利用二维功率谱技术,估计了结构(断层)的深度,并在550 m处检测到浅层侵入。从地震活动性、地表地质、RTP图和钻孔资料等方面评价和讨论了西南-开罗地区的构造格架,并在浅部和深部追踪了活动断裂。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Seismic Risk Zones and Faults Characterization using Geophysical Data
Understanding and imaging the real seismo-tectonic of SW-Cairo zone are essential to eliminate the risk of this hazardous seismic zone which is surrounded by the highest condense population province in Egypt. In this study, up to date earthquake catalogue and aeromagnetic data of the area under study were analyzed for tracing active subsurface faults that are responsible of earthquakes activity. Using 2D-power spectrum techniques, depth of structures (faults) was estimated and a shallow intrusion was detected at 550 m. The tectonic framework of SW-Cairo was evaluated and discussed in view of seismicity, surface geology, subsurface structures from RTP maps and boreholes information and the active faults were traced at shallow and deep depths.
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