Elementary theory of earthquake source relaxation
A.V. Guglielmi

TL;DR
This paper presents an axiomatic elementary theory of earthquake source relaxation, introducing a new concept of source deactivation and revealing a two-stage relaxation process with a bifurcation, challenging classical aftershock laws.
Contribution
It introduces a novel axiomatic framework for earthquake source relaxation, including a new deactivation coefficient and a two-stage relaxation model with bifurcation, expanding theoretical understanding.
Findings
Discovered a two-stage relaxation process with bifurcation.
Classical Omori law is limited to the first relaxation stage.
Hirano-Utsu law does not apply to either relaxation stage.
Abstract
The elementary theory of relaxation of the source cooling down after the main shock of an earthquake is presented axiomatically. The names of the objects under study are given and the relationships between them are determined. A new basic concept of earthquake source deactivation is introduced and a procedure for calculating the deactivation coefficient from aftershock frequency measurement data is indicated. An important property of the system is that the axioms do not contain statements regarding the actual process of source relaxation. From two simple axioms a number of meaningful statements (theorems) logically follow. A two-stage mode of source relaxation was discovered. The sharp transition between stages has the character of a bifurcation. It is shown that the classical Omori law has limited applicability. It describes the evolution of aftershocks only at the first stage of…
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Taxonomy
TopicsEarthquake Detection and Analysis · Geotechnical and Geomechanical Engineering
