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首页> 外文期刊>Natural hazards and earth system sciences >Analysis of the cross-correlation between seismicity and water level in the Aswan area (Egypt) from 1982 to 2010
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Analysis of the cross-correlation between seismicity and water level in the Aswan area (Egypt) from 1982 to 2010

机译:1982年至2010年埃及阿斯旺地区地震活动与水位之间的互相关分析

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摘要

In this study the correlation between the monthly fluctuations of the water level of the Aswan High Dam and monthly number of earthquakes from 1982 to 2010, which occurred in the surrounding area, was investigated. Our findings reveal that significant correlation is present during the period 1982-1993 between water level and shallow seismicity (depth less than 15 km). The deep seismicity (depth larger than 15 km) is significantly correlated with the water level between January and April 1989. The time lag of the significant maximal cross-correlation varies from 2-8 months for the shallow seismicity, while it is around 7-8 months for the deep seismicity. These values of the time lags could be in favour of the presence of two distinct triggering mechanisms: one due to pore pressure diffusion and the other due to fracture compaction (undrained response).
机译:本文研究了1982年至2010年阿斯旺高坝水位每月波动与周围地区每月地震次数之间的相关性。我们的发现表明,在1982-1993年期间,水位与浅层地震活动性(深度小于15 km)之间存在显着相关性。深度地震活动(深度大于15 km)与1989年1月至1989年4月之间的水位显着相关。显着最大互相关的时滞在浅度地震活动中为2-8个月不等,而在7- 8个月的深地震力。时滞的这些值可能有利于存在两种不同的触发机制:一种是由于孔隙压力扩散引起的,另一种是由于裂缝压实(不排水的响应)引起的。

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