2020年3月25日帕拉穆希尔7.5兆瓦地震

A. Prytkov, N. F. Vasilenko
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引用次数: 0

摘要

这场矩震级Mw=7.5的强烈地震发生在2020年3月25日,地点位于帕拉穆希尔岛东南部的北千岛。地震震源位于俯冲太平洋岩石圈板块深海海沟的洋隆下方。这次地震是自1900年以来,海沟外隆起约800公里长地区发生的最强地震事件。这也是震中附近300公里长的千岛-堪察加俯冲带发生的最强地震。本文总结了帕拉穆希尔地震资料。考虑了地震的构造位置、震源参数、余震过程发展特征以及最近连续GNSS站的同震位移。所进行的分析使我们无法清楚地确定震源中的破裂面。然而,研究外升地震的特征是一个具有科学意义的问题,因为俯冲太平洋岩石圈板块弯曲区的应力状态反映了俯冲带中板间的相互作用。
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The March 25, 2020 MW 7.5 Paramushir earthquake
The strong earthquake with moment magnitude Mw = 7.5 occurred on March 25, 2020, in the North Kurils to the southeast of the Paramushir Island. The hypocenter of the earthquake was located under the oceanic rise of deep-sea trench in the subducting Pacific lithospheric plate. This earthquake has been the strongest seismic event since 1900 for an area about 800 km long of the outer rise of the trench. It also was the strongest earthquake for the 300-kilometer long area of the Kuril-Kamchatka subduction zone adjacent to the epicenter. The article summarizes the data on the Paramushir earthquake. Tectonic position of the earthquake, source parameters, features of the aftershock process development, as well as coseismic displacement of the nearest continuous GNSS station are considered. The performed analysis did not allow us to clearly determine the rupture plane in the source. Nevertheless, the study of the features of the outer-rise earthquake is a matter of scientific interest, since the stress state of the bending area of the subducting Pacific lithospheric plate reflects the interplate interaction in the subduction zone.
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