欧洲-非洲经构造带区域生震构造的比较特征

Viktor A. Ogadzhanov
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引用次数: 0

摘要

根据新的地震活动性数据和活动断层调查资料,获得了欧洲-非洲通构造带区域发震构造的信息。给出了构成贯通构造带的断层的运动特征以及在这些构造中发生的地震。基于卫星数据的重力异常分析表明,欧洲-非洲穿过构造带的发震构造在地幔中具有超深的渗透,这决定了它们的高地震潜力。这种潜力在2023年2月6日地中海-里海地区的灾难性地震中得到了体现。2023年2月6日地震后,在高加索褶皱构造和东欧地台地区,地震活动向东北方向偏移。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Comparative characteristic of regional seismo-generating structures of the EuropeanAfrican through tectonic belt
Based on new data on seismicity and materials from surveys of active faults, information was obtained on regional seismogenic structures of the European-African through tectonic belt. The kinematic characteristics of the faults that make up the through tectonic belt and earthquakes that occurred within these structures are given. An analysis of gravity anomalies based on satellite data suggests that the seismogenic structures of the European -African through tectonic belt have an ultra-deep penetration into the mantle, which determines their high seismic potential. This potential was manifested by catastrophic earthquakes in the Mediterranean-Caspian region on February 6, 2023. Afterthe earthquakes onFebruary 6, 2023,themigration ofseismic activity inthe northeast direction, inthe area ofthe Caucasus fold structure and the East European platform, was noted.
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