Numerical models of earthquake mechanism

The tectonic creep and its variation after particular earthquakes are studied by the Stokes equation. The stress state of the region is modelled according to a hypothesis of plate tectonics in which the lithosphere of the region is laterally compressed across the Eurasian, Indian, and Arabian plates...

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Main Author: Ikram Atabekov
Format: Article
Language:English
Published: KeAi Communications Co., Ltd. 2021-03-01
Series:Geodesy and Geodynamics
Subjects:
Online Access:http://www.sciencedirect.com/science/article/pii/S1674984721000173
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author Ikram Atabekov
author_facet Ikram Atabekov
author_sort Ikram Atabekov
collection DOAJ
description The tectonic creep and its variation after particular earthquakes are studied by the Stokes equation. The stress state of the region is modelled according to a hypothesis of plate tectonics in which the lithosphere of the region is laterally compressed across the Eurasian, Indian, and Arabian plates. The 1966 Tashkent (Uzbekistan) earthquake and the 1976 Gazli (Uzbekistan) earthquake are selected as examples to study different models of earthquake focal mechanisms. Based on the specifics of the geodynamic formulation, the three-dimensional equations of moment elasticity and hydromechanics are reduced to two-dimensional equations for averaged stresses, displacements, and displacement velocities. The two-dimensional equations are solved by boundary integral equations. The stresses can be useful in zoning maps. The vertical velocities obtained from the creep model of the earth's crust can serve as additional data to Central Asia's horizontal velocities from GPS measurements.
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spelling doaj.art-647a4193f8dd478abf6eca726124197f2022-12-21T22:42:46ZengKeAi Communications Co., Ltd.Geodesy and Geodynamics1674-98472021-03-01122148154Numerical models of earthquake mechanismIkram Atabekov0Institute of Seismology, Tashkent, 100128, UzbekistanThe tectonic creep and its variation after particular earthquakes are studied by the Stokes equation. The stress state of the region is modelled according to a hypothesis of plate tectonics in which the lithosphere of the region is laterally compressed across the Eurasian, Indian, and Arabian plates. The 1966 Tashkent (Uzbekistan) earthquake and the 1976 Gazli (Uzbekistan) earthquake are selected as examples to study different models of earthquake focal mechanisms. Based on the specifics of the geodynamic formulation, the three-dimensional equations of moment elasticity and hydromechanics are reduced to two-dimensional equations for averaged stresses, displacements, and displacement velocities. The two-dimensional equations are solved by boundary integral equations. The stresses can be useful in zoning maps. The vertical velocities obtained from the creep model of the earth's crust can serve as additional data to Central Asia's horizontal velocities from GPS measurements.http://www.sciencedirect.com/science/article/pii/S1674984721000173Central AsiaStress stateEarthquake mechanismNumerical modelBoundary element method
spellingShingle Ikram Atabekov
Numerical models of earthquake mechanism
Geodesy and Geodynamics
Central Asia
Stress state
Earthquake mechanism
Numerical model
Boundary element method
title Numerical models of earthquake mechanism
title_full Numerical models of earthquake mechanism
title_fullStr Numerical models of earthquake mechanism
title_full_unstemmed Numerical models of earthquake mechanism
title_short Numerical models of earthquake mechanism
title_sort numerical models of earthquake mechanism
topic Central Asia
Stress state
Earthquake mechanism
Numerical model
Boundary element method
url http://www.sciencedirect.com/science/article/pii/S1674984721000173
work_keys_str_mv AT ikramatabekov numericalmodelsofearthquakemechanism