Abstract
The aim of this study is to demonstrate how the 12 October 1992 Cairo earthquake relates to the spatial geometry of the northern Egyptian fault systems. A box-counting algorithm was used, in a focused down approach (from regional to local scales) to analyze the fractal dimensions of the existing faults. The results indicate that these faults display fractal geometries that are self-similar over two to three orders of magnitude. It is shown that the northwest-southeast (Northern Red Sea) trending fault system has the lowest fractal dimension value. Coincidentally, this fault trend is the one that the fault plane solution shows to be active.
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Arab, N., Kazi, A. & Rieke, H.H. Fractal geometry of faults in relation to the 12 October 1992 Cairo earthquake. Nat Hazards 10, 221–233 (1994). https://doi.org/10.1007/BF00596143
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DOI: https://doi.org/10.1007/BF00596143