1999年8月17日İzmit地震前后南马尔马拉地区(t rkiye)的地震活动

M. Utkucu, Fatih Uzunca, H. Durmuş, Serap Kırım, S. Nalbant
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引用次数: 0

摘要

本文对1999年İzmit地震前后马尔马拉南部地区的地震活动性进行了分析和比较。采用了完整度在MC=2.9以上的均匀地震活动目录,涵盖了1978年至2020年的时间段。1999年İzmit地震前后的频率-震级分布空间图对比显示,地震后b值普遍增大,表明该地区应力总体减小。1999年地震后,布尔萨市东部约450年的最短计算TL值消失了。b值的计算时间变化在1978 - 1997年间从0.8增加到1.6,在2000 - 2006年间从1.1增加到2.1。2006年以后,b值从2.1下降到0.8,说明1999年İzmit地震后的应力下降在该年后开始增加。由于历史上的地震活动表明,沿着Geyve城镇延伸的北安那托利亚断裂带的断层段没有发生大地震,İznik, Gemlik和Bandırma被认为是最有可能在该地区发生下一次破坏性地震的断层。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Seismicity of the Southern Marmara Region (Türkiye) before and after the August 17, 1999 İzmit earthquake
In the present study seismicity of the Southern Marmara Region before and after the 1999 İzmit earthquake are analyzed and compared. A homogeneous seismicity catalogue that have completeness above the MC=2.9 and covers the time period between 1978 and 2020 is used. Comparison of the spatial mapping of the frequency-magnitude distribution before and after the 1999 İzmit earthquake revealed that b-values demonstrate a general increase after the earthquake indicating a general stress decrease in the region. The shortest computed TL value of about 450 years in the east of city of Bursa vanished after the 1999 earthquake. The computed time variations of b-value have shown an increase from 0.8 to 1.6 between 1978 and 1997 and an anomalous increase from 1.1 to 2.1 between 2000 and 2006. After 2006, b-values have decreased from 2.1 to 0.8, implying that decreased stress after the 1999 İzmit earthquake begun to increase after that year. Since the historical seismicity indicates no large earthquake on the fault segments of the North Anatolian Fault Zone extending along the towns of Geyve, İznik, Gemlik and Bandırma are considered to be most likely faults to host the next destructive earthquakes in the region.
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