南堪察加环形地震活动性结构:大地震的可能准备

IF 1 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS
Yu. F. Kopnichev, I. N. Sokolova
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引用次数: 0

摘要

文摘:讨论了南堪察加地震活动性的一些特征。研究了2024年8月17日7.0级大地震的余震云参数。结果表明,堪察加南部在0 ~ 33、34 ~ 70、71 ~ 110 km三个深度范围内形成了环形地震活动构造。与其他俯冲带一样,该构造的特征是根据极限震级(分别为Mt1、Mt2和Mt3)和长轴L1、L2和L3的长度来确定的。2024年8月17日的地震及其最强余震的震中位于一个浅环形结构(Mt1 = 5.3),这支持了南堪察加地区准备发生大地震的假设。在以前的工作中,已经构造了参数Mt1和Mt2与西太平洋(Mw = 7.0-9.0)大地震Mw级的相关依赖关系。利用这些依赖关系,我们估计该地区可能发生的大事件的震级为Mw = 8.6±0.2。讨论了俯冲带不同深度环形地震活动性构造形成的因素。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Ring-Shaped Seismicity Structures in South Kamchatka: Probable Preparation of a Great Earthquake

Ring-Shaped Seismicity Structures in South Kamchatka: Probable Preparation of a Great Earthquake

Abstract—Some characteristics of seismicity in South Kamchatka are discussed. Parameters of the aftershock cloud of the August 17, 2024 large earthquake (Mw = 7.0) are studied. It is shown that ring-shaped seismicity structures in South Kamchatka have been formed in three depth ranges: 0–33, 34–70, and 71–110 km. As in other subduction zones, the structures are characterized in terms of limiting magnitude values—threshold magnitudes Mt1, Mt2, and Mt3, respectively, and lengths of major axes L1, L2, and L3. The epicenters of the August 17, 2024 earthquake and its strongest aftershocks fall in a shallow ring-shaped structure (Mt1 = 5.3), which supports the hypothesis of a preparation of a great earthquake in the South Kamchatka region. In the previous works, the correlation dependences of parameters Mt1 and Mt2 on the magnitudes Mw of large earthquakes have been constructed for the western Pacific (in the range Mw = 7.0–9.0). Using these dependencies, we estimated the magnitude of the great possible event in this region at Mw = 8.6 ± 0.2. The factors responsible for the formation of ring-shaped seismicity structures at different depths in the subduction zones are discussed.

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来源期刊
Izvestiya, Physics of the Solid Earth
Izvestiya, Physics of the Solid Earth 地学-地球化学与地球物理
CiteScore
1.60
自引率
30.00%
发文量
60
审稿时长
6-12 weeks
期刊介绍: Izvestiya, Physics of the Solid Earth is an international peer reviewed journal that publishes results of original theoretical and experimental research in relevant areas of the physics of the Earth''s interior and applied geophysics. The journal welcomes manuscripts from all countries in the English or Russian language.
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