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首页> 外文期刊>Pure and Applied Geophysics >Influence of Rivera-Cocos plate boundary geodynamics on earthquake intensity patterns: The 9 October 1995 (Mw 8.0) and 21 (22) January 2003 (Mw 7.5) earthquakes
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Influence of Rivera-Cocos plate boundary geodynamics on earthquake intensity patterns: The 9 October 1995 (Mw 8.0) and 21 (22) January 2003 (Mw 7.5) earthquakes

机译:Rivera-Cocos板块边界动力学对地震烈度分布的影响:1995年10月9日(Mw 8.0)和2003年1月21日(22)(Mw 7.5)地震

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摘要

This study examines two large thrust subduction earthquakes occurring within the Rivera-Cocos plate boundary which struck the western coast of México on 9 October 1995, Mw 8.0, and 21 (22 GMT) January 2003, Mw 7.5. The Modified Mercalli (MM) earthquake intensities observed during theseearthquakes were surprising for some towns located in the Mexican coastal zone. During the smaller Mw 7.5 2003 earthquake, MM intensity VII was observed for towns of Colima, Villa de Alvarez and Ixtlahuacán, while during the larger Mw 8.0 1995 earthquake, their MM intensities were only IV-V, V and V-VI, respectively. We construct the macroseismic patterns for these two earthquakes and discuss the possible reasons for the significant difference in the outline of the MM VII isoseismals, such as the tectonic setting of epicentral zones and the directivity of rupture processes along and across the coastal line.
机译:这项研究调查了发生在1995年10月9日Mw 8.0和21(22 GMT)Mw 7.5的墨西哥西部海岸的Rivera-Cocos板块边界内发生的两次大的逆冲俯冲地震。在这些地震期间观察到的修正的Mercalli(MM)地震烈度,对于墨西哥沿海地区的一些城镇来说是令人惊讶的。在较小的2003年Mw 7.5地震中,科利马,Villa de Alvarez和伊斯塔拉瓦坎的城镇观测到MM强度VII,而在1995年8.0较大的地震中,它们的MM强度分别仅为IV-V,V和V-VI。我们构造了这两次地震的大震模式,并讨论了MM VII等震线轮廓存在重大差异的可能原因,例如震中区的构造背景以及沿海岸线和跨海岸线的破裂过程的方向性。

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