A SERIES of TANGIBLE EARTHQUAKES in 2018–2019 in the FOCAL ZONE of the 10-point SPITAK EARTHQUAKE of 1988

G.V. Sargsyan, G.R. Abgaryan, A.A. Grigoryan, N. Petrova
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Abstract

The paper presents the results of a study of 2018–2019 tangible seismic events with intensity at the epicenter of 5–6 points and above, that occurred in the focal zone of the 10-point Spitak earthquake of 07.12.1988 with MLH =6.8. Two earthquakes of June 6, 2018, with МL=3.6 and МL=4.3, as well as two shocks on September 10, 2019, with МL=4.7 and with МL=3.9, were felt in the nearest settlements with an intensity of 5 or more points. For three of them, according to the collected macroseismic data, isoseist maps were constructed and macroseismic parameters were determined. The strike of the nodal planes in the earthquake sources is consistent with the direction of elongation of the isoseist system, which, in turn, for three events coincides with the strike of the nearest faults of the Pambak-Sevan system.
2018-2019 年在 1988 年 10 点 SPITAK 地震中心区发生的一系列有形地震
本文介绍了2018-2019年发生在1988年12月7日MLH=6.8的斯皮塔克10点地震焦点区的震中烈度为5-6点及以上的有形地震事件的研究结果。2018 年 6 月 6 日发生的МL=3.6 和МL=4.3 的两次地震,以及 2019 年 9 月 10 日发生的МL=4.7 和МL=3.9 的两次地震,在最近的居民点都有震感,烈度在 5 点及以上。根据收集到的宏观地震数据,为其中三个定居点绘制了等深线图,并确定了宏观地震参数。震源节点平面的走向与等深线系统的延伸方向一致,而三个事件的等深线系统又与最近的 Pambak-Sevan 系统断层的走向相吻合。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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