Dependence of the source deactivation factor on the earthquake magnitude
A.V. Guglielmi, O.D. Zotov

TL;DR
This paper introduces a differential model to analyze how the earthquake source deactivation factor varies with main shock magnitude, offering new insights into well-known seismic laws and addressing energy conservation issues.
Contribution
It proposes a novel differential equation framework for earthquake aftershock dynamics, revealing the dependence of the deactivation factor on main shock magnitude.
Findings
Deactivation factor decreases monotonically with increasing main shock magnitude.
The model successfully explains the evolution of aftershock activity.
It offers a way to reconcile Omori's law with energy conservation principles.
Abstract
Three fundamental laws of the physics of earthquakes, bearing the names of their discoverers Omori, Gutenberg, Richter and Bath, are widely used in original, review, monographic, and encyclopedic literature. In this paper, we have tried to look at laws from an unusual point of view. The idea behind our approach is as follows. Each of the three laws was established in the course of work on solving a specific research problem, and the result was expressed in a specific mathematical form. We asked ourselves whether it is possible to modify the statement of the problem, and/or modify the form of expression of the law in order to see new facets of a well-known scientific statement? The result was successful in relation to Omori's law, according to which the frequency of aftershocks hyperbolically decreases over time. The modified formulation of the problem was to find a differential equation…
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Taxonomy
Topicsearthquake and tectonic studies · Earthquake Detection and Analysis · High-pressure geophysics and materials
