SARIKHOSOR EARTHQUAKES on March 29, 2018 with KR=13.1, Мs=5.1, I0=6 and March 7, 2019 with KR=12.1, МS=4.1, I0=5–6 (Tajikistan)

R. U. Juraev
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Abstract

General information about the tangible earthquakes that occurred on the territory of Tajikistan in 2018–2019 and their confinement to tectonic structures is given. The most active tectonic structures during this period within which strong seismic events occurred are determined. The results of a survey of macroseismic manifestations of March 29, 2018 and March 7, 2019 earthquakes, which occurred in the eastern part of the Tajik depression, and their isoseist maps are presented. An assumption about the possible influence of two large reservoirs on the increase of the seismicity of the region is made. An analysis of the depths of earthquake sources in comparison with the geological and tectonic structures of the region is made. The difference in the depths of earthquakes, determined by different seismological services, makes it difficult to link the source of seismic events to tectonic structures and to determine their parameters.
SARIKHOSOR 地震,2018 年 3 月 29 日 KR=13.1,МS=5.1,I0=6;2019 年 3 月 7 日 KR=12.1,МS=4.1,I0=5-6(塔吉克斯坦)。
本文介绍了 2018-2019 年塔吉克斯坦境内发生的有形地震的一般信息及其与构造结构的关系。确定了在此期间发生强震事件的最活跃构造结构。介绍了 2018 年 3 月 29 日和 2019 年 3 月 7 日发生在塔吉克洼地东部的地震的宏观地震表现调查结果及其等震源图。假设两个大型水库可能对该地区地震的增加产生影响。分析了地震源深度与该地区地质和构造结构的对比。由于不同地震部门确定的地震深度不同,很难将地震事件的震源与构造结构联系起来并确定其参数。
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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