EARTHQUAKE of APRIL 24, 2018 with KR=10.5, Мw3.9 and I0=5 in the ANAPA-NOVOROSSIYSK ZONE

A. I. Klyanchin, A. Zvereva, I. Gabsatarova
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Abstract

The article presents instrumental and macroseismic data on the earthquake of April 24, 2018 with Мw=3.9, which occurred at the Black Sea coast near the Abrau Peninsula. The earthquake was felt in 15 settlements at distances up to 52 km from the epicenter with an intensity of 3 to 5 points. The earthquake occurred in the Black Sea zone of occurrence of earthquakes. The scalar seismic moment М0 and the spectral moment magnitude Mw=3.9 were calculated based on the spectra of seven regional stations. The focal mechanism was constructed based on the signs of the first movement in the P-wave at 68 stations. It is established that a thrust has occurred in the source along a northwest-trending plane dipping to the northeast, which is consistent with the orientation and dip of the fault planes of tectonic structures in the area of the source. The macroseismic manifestations of the April 24, 2018 earthquake made it possible to choose the most acceptable depth value and calculate the intensity at the epicenter (h=10 km, I0=5)
2018年4月24日在安纳帕-诺沃罗西斯克地区发生的地震,KR=10.5,Мw3.9,I0=5
文章介绍了 2018 年 4 月 24 日发生在黑海沿岸阿布劳半岛附近的Мw=3.9 地震的仪器和宏观地震数据。距离震中 52 千米的 15 个居民点均有震感,烈度为 3 至 5 级。地震发生在黑海地震多发区。根据七个地区台站的频谱计算了标量地震力矩 М0和频谱地震力矩震级 Mw=3.9。根据 68 个台站 P 波第一次运动的迹象,构建了焦点机制。结果表明,震源发生了沿西北向平面向东北倾斜的推力,这与震源地区构造结构断层面的走向和倾角一致。2018 年 4 月 24 日地震的宏观地震表现使得选择最可接受的深度值和计算震中烈度(h=10 千米,I0=5)成为可能
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