2018 年 9 月 4 日卡塔夫-伊万诺夫斯克地震,ML=5.4,mb=5.5,I0=6.4

F. Verkholantsev, R. Diagilev, D. Shulakov, Yuliya V. Varlashova
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引用次数: 0

摘要

本文介绍了 2018 年 9 月 4 日 22 时 58 分 19 秒(世界协调时)在车里雅宾斯克州(南乌拉尔)卡塔夫-伊万诺夫斯克市附近发生的地震的仪器数据和宏观地震数据,ML=5.4,I0=6.4±0.3。这次 ML=5.4 mb=5.5 的地震成为乌拉尔地区有仪器记录的最强地震,在 2018 年俄罗斯地震中具有最高的宏观地震效应(I0=6.4±0.3)。在处理乌拉尔地区宏观地震数据的实践中,首次使用了 2017 年地震烈度表(GOST R 57546-2017)。在乌拉尔地区的天然地震中,首次记录了余震过程,其活跃阶段持续了约 11 个月,而许多余震具有显著的宏观地震效应。考虑到余震云的空间方位,确认了焦点机制解决方案,并证实了震源的构造位置。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
SEPTEMBER 4, 2018 KATAV-IVANOVSK EARTHQUAKE with ML=5.4, mb=5.5, I0=6.4
The instrumental and macroseismic data on the earthquake of September 4, 2018 at 22h58m19s UTC, ML=5.4, I0=6.4±0.3 near the city of Katav-Ivanovsk in the Chelyabinsk region (South Urals) are presented. This event with ML=5.4 mb=5.5 became the strongest instrumentally recorded earthquake in the Urals and had the highest macroseismic effect among the Russian earthquakes in 2018 (I0=6.4±0.3). For the first time in the practice of processing macroseismic data in the Urals, the Seismic Intensity Scale 2017 (GOST R 57546-2017) was used. For the first time for natural earthquakes in the Urals, an aftershock process was recorded, the active stage of which lasted about 11 months, while many aftershocks had a significant macroseismic effect. Taking into account the spatial orientation of the aftershock cloud, the focal mechanism solution was confirmed and the tectonic position of the source was substantiated.
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