Uber seismische Wellen in nnelastischcni Material

SUMMARY - The propagation of seismic waves in inelastic media is investigated.<br />The relation between stress and strain tensor is of the form<br />7 OV; + Ptj = U' Ekk Sij + z V + A £kk Sii + z (" Eii<br />Tehe velocity of propagation and the ex...

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Main Author: H. MENZEL
Format: Article
Language:English
Published: Istituto Nazionale di Geofisica e Vulcanologia (INGV) 1977-06-01
Series:Annals of Geophysics
Online Access:http://www.annalsofgeophysics.eu/index.php/annals/article/view/4824
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spelling doaj-04f564588e43421e9cc38a4e2beceaa32020-11-25T00:45:19ZengIstituto Nazionale di Geofisica e Vulcanologia (INGV)Annals of Geophysics1593-52132037-416X1977-06-01303-428529810.4401/ag-4824Uber seismische Wellen in nnelastischcni MaterialH. MENZELSUMMARY - The propagation of seismic waves in inelastic media is investigated.<br />The relation between stress and strain tensor is of the form<br />7 OV; + Ptj = U' Ekk Sij + z V + A £kk Sii + z (" Eii<br />Tehe velocity of propagation and the extinction both of compressional and<br />shear-waves are calculated. The exitation of the waves is assumed to be purely<br />harmonic and acting at a line of the surface.http://www.annalsofgeophysics.eu/index.php/annals/article/view/4824
collection DOAJ
language English
format Article
sources DOAJ
author H. MENZEL
spellingShingle H. MENZEL
Uber seismische Wellen in nnelastischcni Material
Annals of Geophysics
author_facet H. MENZEL
author_sort H. MENZEL
title Uber seismische Wellen in nnelastischcni Material
title_short Uber seismische Wellen in nnelastischcni Material
title_full Uber seismische Wellen in nnelastischcni Material
title_fullStr Uber seismische Wellen in nnelastischcni Material
title_full_unstemmed Uber seismische Wellen in nnelastischcni Material
title_sort uber seismische wellen in nnelastischcni material
publisher Istituto Nazionale di Geofisica e Vulcanologia (INGV)
series Annals of Geophysics
issn 1593-5213
2037-416X
publishDate 1977-06-01
description SUMMARY - The propagation of seismic waves in inelastic media is investigated.<br />The relation between stress and strain tensor is of the form<br />7 OV; + Ptj = U' Ekk Sij + z V + A £kk Sii + z (" Eii<br />Tehe velocity of propagation and the extinction both of compressional and<br />shear-waves are calculated. The exitation of the waves is assumed to be purely<br />harmonic and acting at a line of the surface.
url http://www.annalsofgeophysics.eu/index.php/annals/article/view/4824
work_keys_str_mv AT hmenzel uberseismischewelleninnnelastischcnimaterial
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