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首页> 外文期刊>Journal of Seismology >Mapping of b-values, earthquake relocation, and Coulomb stress changes during 1992–2007 in the Murindó seismic zone, Colombia
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Mapping of b-values, earthquake relocation, and Coulomb stress changes during 1992–2007 in the Murindó seismic zone, Colombia

机译:哥伦比亚Murindó地震带在1992-2007年间的b值映射,地震迁移和库仑应力变化

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Seismicity in the Murindó seismic zone, Colombia (6° to 8° and − 75.5° to − 78.0°) during 1992–2007 included the occurrence of the M W 6.6 foreshock on October 17, and M W 7.1 mainshock on October 18, 1992, and aftershocks, which caused severe damage throughout the region. We modeled this seismic sequence by means of Coulomb stress changes imparted by slip along two semi-vertical fault planes with left-lateral motion and subdivided slip. Seismicity thereafter (1993–2007) was characterized by earthquakes magnitude in the range 0.7−6.1 for which a magnitude of completeness M C = 2.7 was determined. b-values are relatively high to the south of the study region and relatively low to the north and northwest. The relocation of epicenters indicates that recent seismicity may be occurring on a fault that is yet to be mapped under the Atrato river valley. We conclude that the 1992 seismic sequence was a case of a major earthquake facilitated by the stress changes imparted during a strong rupture the previous day and that the aftershocks and background seismicity in the region can be explained by static Coulomb stress changes up to 50.1 bar. Our results have implications for hazard in Colombia and serve as basis to foster future investigations.
机译:在1992–2007年期间,哥伦比亚Murindó地震带(6°至8°,− 75.5°至− 78.0°)的地震活动包括10月17日发生了M W 6.6前震,M < Sub> W 7.1于1992年10月18日发生主震,并发生余震,对整个地区造成了严重破坏。我们通过库仑应力变化对这种地震序列进行了建模,库仑应力变化是由沿两个半垂直断层的滑移产生的,具有左旋运动和细分滑移。此后(1993-2007年)的地震活动的特征是震级在0.7-6.1之间,确定的震级M C = 2.7。 b值在研究区域的南部相对较高,而在北部和西北部则相对较低。震中的重新定位表明,最近的地震活动可能发生在尚未绘制在阿特拉托河谷下方的断层上。我们得出的结论是,1992年的地震序列是大地震的一个例子,前一天发生的强烈破裂赋予了应力变化,而该区域的余震和背景地震活动可以用高达50.1 bar的静态库仑应力变化来解释。我们的结果对哥伦比亚的危害具有影响,并为促进未来的调查奠定了基础。

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