On estimation of the displacement in an earthquake source and of source dimensions

The study of an earthquakes mechanism is usually fìnished bythe determination of a fault piane and the direction of displacementalong it. In many aspects of geodynamics and seismology it wouldbe very important to estimate also the dimensions of a source and cliiefly— the magnitude of the displacemen...

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Main Author: V. K. Borok
Format: Article
Language:English
Published: Istituto Nazionale di Geofisica e Vulcanologia (INGV) 1959-06-01
Series:Annals of Geophysics
Online Access:http://www.annalsofgeophysics.eu/index.php/annals/article/view/5718
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spelling doaj-50e4c8a918a444d980f21e572703a5d62020-11-25T00:36:34ZengIstituto Nazionale di Geofisica e Vulcanologia (INGV)Annals of Geophysics1593-52132037-416X1959-06-0112220521410.4401/ag-5718On estimation of the displacement in an earthquake source and of source dimensionsV. K. BorokThe study of an earthquakes mechanism is usually fìnished bythe determination of a fault piane and the direction of displacementalong it. In many aspects of geodynamics and seismology it wouldbe very important to estimate also the dimensions of a source and cliiefly— the magnitude of the displacement in it.This problem can be reduced to the comparing of fields of sfaticaistress before an earthquake and after it. The difference of energies ofthese two fields depends upon source properties in question; lience it ispossible to determine dimensions of the source and the displacementin it if the forni of the source and the difference of the energies be known.The energy difference can be found from observations on the seismicwaves energy.The idea of such an approach belongs to L. Knopoff. He solved thetwo — dimensionai problem which. deals with the study of very strongearthquakes with long faults. The analogica! three — dimensionaiproblem is considered in this paper; it is necessary for studying of morenumerous weaker earthquakes and investigation of some contiguousproblema.http://www.annalsofgeophysics.eu/index.php/annals/article/view/5718
collection DOAJ
language English
format Article
sources DOAJ
author V. K. Borok
spellingShingle V. K. Borok
On estimation of the displacement in an earthquake source and of source dimensions
Annals of Geophysics
author_facet V. K. Borok
author_sort V. K. Borok
title On estimation of the displacement in an earthquake source and of source dimensions
title_short On estimation of the displacement in an earthquake source and of source dimensions
title_full On estimation of the displacement in an earthquake source and of source dimensions
title_fullStr On estimation of the displacement in an earthquake source and of source dimensions
title_full_unstemmed On estimation of the displacement in an earthquake source and of source dimensions
title_sort on estimation of the displacement in an earthquake source and of source dimensions
publisher Istituto Nazionale di Geofisica e Vulcanologia (INGV)
series Annals of Geophysics
issn 1593-5213
2037-416X
publishDate 1959-06-01
description The study of an earthquakes mechanism is usually fìnished bythe determination of a fault piane and the direction of displacementalong it. In many aspects of geodynamics and seismology it wouldbe very important to estimate also the dimensions of a source and cliiefly— the magnitude of the displacement in it.This problem can be reduced to the comparing of fields of sfaticaistress before an earthquake and after it. The difference of energies ofthese two fields depends upon source properties in question; lience it ispossible to determine dimensions of the source and the displacementin it if the forni of the source and the difference of the energies be known.The energy difference can be found from observations on the seismicwaves energy.The idea of such an approach belongs to L. Knopoff. He solved thetwo — dimensionai problem which. deals with the study of very strongearthquakes with long faults. The analogica! three — dimensionaiproblem is considered in this paper; it is necessary for studying of morenumerous weaker earthquakes and investigation of some contiguousproblema.
url http://www.annalsofgeophysics.eu/index.php/annals/article/view/5718
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