研究描述余震的平野宇津定律真假的公理方法

A. V. Guglielmi
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摘要

余震演化幂律由平野(Hirano)于 1924 年提出,Utsu 在上世纪下半叶将其引入地震学。平野-宇津定律被广泛用于研究地震主震后震源的松弛。文献中普遍认为平野宇津定律是 1894 年提出的大森双曲线定律的改进版。作者不同意这种观点。本文提出了一种研究余震的公理方法。文中引入了一个震源的现象学参数,称为失活系数。该理论以公理为基础,不包含任何关于余震演变规律形式的先验陈述。根据公理推导出了失活系数公式,从而可以通过实验确定平野宇津定律和大森定律的真假。我们发现了源松弛的两阶段模式。第一阶段称为大森纪元,严格遵循大森定律。大森周期以断裂结束,之后余震活动变得不可预测。大森定律在演化的第二阶段并不适用。平野宇津定律在第一阶段和第二阶段都没有得到满足。关键词:震源、主震、弛豫、失活系数、演化方程、逆问题、大森纪元、分岔、两阶段弛豫模式。
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An axiomatic method for studying the truth or falsity of the Hirano-Utsu law describing aftershocks
The power law of aftershock evolution was proposed by Hirano in 1924 and introduced by Utsu into seismology in the second half of the last century. The Hirano-Utsu law is widely used in studying the relaxation of earthquake source after the main shock of an earthquake. The prevailing view in the literature is that the Hirano-Utsu law is an improved version of Omori's hyperbolic law, formulated in 1894. The author disagrees with this notion. The paper proposes an axiomatic approach to the study of aftershocks. A phenomenological parameter of the source, called the deactivation coefficient, was introduced. The theory is based on axioms that do not contain any a priori statements regarding the form of the law of aftershock evolution. Formulas for the deactivation coefficient are derived from the axioms, allowing one to experimentally establish the truth or falsity of the Hirano-Utsu and Omori laws. A two-stage mode of source relaxation was discovered. In the first stage, called the Omori epoch, the Omori law is strictly followed. The Omori epoch ends with a bifurcation, after which aftershock activity becomes unpredictable. Omori's law is not fulfilled at the second stage of evolution. The Hirano-Utsu law is not fulfilled either at the first or second stage. Keywords: earthquake source, main shock, relaxation, deactivation coefficient, evolution equation, inverse problem, Omori epoch, bifurcation, two-stage relaxation mode.
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