Instanton Representation of Foreshoсk–Aftershock Sequences

IF 1 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS
L. M. Bogomolov, M. V. Rodkin, V. N. Sychev
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引用次数: 0

Abstract—The description of foreshock and aftershock activation processes is of great significance in seismology both from practical and theoretical standpoints. An analogy between the mathematical expressions describing the seismicity patterns in the direct and inverse Omori–Utsu laws has been empirically established. Studies of the generalized vicinity of a large earthquake (LEGV, also abbreviated as GVLE) revealed an even closer analogy between the properties of foreshocks and aftershocks. This analogy also holds for the characteristics of the activation process, in particular, for the anomalous changes in the Gutenberg–Richter b-value. We propose a unifying model for the entire foreshock–aftershock process, which is described by kinetic equations with solutions in the form of strongly temporally localized maxima, called instantons by analogy with solitons for lozalized waves. A demonstrating example of an instanton solution is a graph of the time derivative of the logistic dependence describing a transient process. The rate of this process initially increases significantly, reaches a peak, and then asymptotically decreases to zero. The aim of this paper is to demonstrate effectiveness of the instanton model which generalizes the self-developing process (SDP) model but does not involve the formation of a physically unrealizable singularity typically simulating the explosive growth in the number of foreshocks and aftershocks in the vicinity of the main event. The new model is compared with empirical data from the earthquakes that occurred between 2003 and 2023 in the southern part of Sakhalin, an area with the best capabilities for seismicity recording. A reasonable consistency between theoretical and empirical time dependences is obtained both for the LEGV constructed for a region within 44.5°–50.5° N and 141.5°–143.5° E and for separate strong Sakhalin earthquakes.

Abstract Image

前震-余震序列的瞬态表示
前震和余震活化过程的描述在地震学中具有重要的理论和实践意义。在经验上建立了描述大森- utsu正逆规律中地震活动性模式的数学表达式之间的类比。对大地震广义邻近区(LEGV,也缩写为GVLE)的研究揭示了前震和余震性质之间更接近的相似之处。这种类比也适用于激活过程的特征,特别是古腾堡-里希特b值的异常变化。我们为整个前震-余震过程提出了一个统一的模型,该模型用动力学方程来描述,其解以强时间局域极大值的形式出现,称为瞬子,类比于局部化波的孤子。瞬态解的一个演示示例是描述瞬态过程的逻辑依赖的时间导数图。该过程的速率最初显著增加,达到峰值,然后逐渐减小到零。本文的目的是证明瞬时模型的有效性,该模型推广了自发展过程(SDP)模型,但不涉及物理上不可实现的奇点的形成,通常模拟主震附近前震和余震数量的爆炸性增长。新模型与2003年至2023年间发生在库页岛南部的地震的经验数据进行了比较,该地区具有最好的地震活动记录能力。对于在44.5°-50.5°N和141.5°-143.5°E范围内构建的LEGV以及单独的库页岛强地震,理论和经验时间依赖性之间都获得了合理的一致性。
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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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