Zobrazeno 1 - 10
of 35
pro vyhledávání: '"post seismic relaxation"'
Autor:
Mikhail V. Rodkin, Vladimir I. Kaftan
Publikováno v:
Geodesy and Geodynamics, Vol 8, Iss 1, Pp 13-16 (2017)
We have examined the aftershock sequence and the post-seismic deformation process of the Parkfield earthquake (2004, M = 6, California, USA) source area using GPS data. This event was chosen because of the possibility of joint analysis of data from t
Externí odkaz:
https://doaj.org/article/21cb13435afc4d02b0e4acb7832a36cb
Autor:
Filippos Vallianatos, Vassilis Sakkas
Publikováno v:
Applied Sciences, Vol 11, Iss 11, p 4817 (2021)
In the present work, a multiscale post-seismic relaxation mechanism, based on the existence of a distribution in relaxation time, is presented. Assuming an Arrhenius dependence of the relaxation time with uniform distributed activation energy in a me
Externí odkaz:
https://doaj.org/article/592ebf555b12441ea622c220c5e0567c
Publikováno v:
Annals of Geophysics, Vol 53, Iss 2, Pp 89-99 (2010)
We performed an analysis of post-seismic stress relaxation, taking into account generalized linear rheologies. We compared the stress field (and its derived functions) obtained with a classical Maxwell rheology with that obtained with a transient Bur
Externí odkaz:
https://doaj.org/article/74fe63ff38df42aaaa78f108fbaa6aec
Autor:
Vassilis Sakkas, Filippos Vallianatos
Publikováno v:
Applied Sciences
Volume 11
Issue 11
Applied Sciences, Vol 11, Iss 4817, p 4817 (2021)
Volume 11
Issue 11
Applied Sciences, Vol 11, Iss 4817, p 4817 (2021)
In the present work, a multiscale post-seismic relaxation mechanism, based on the existence of a distribution in relaxation time, is presented. Assuming an Arrhenius dependence of the relaxation time with uniform distributed activation energy in a me
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b62db1fe361de9df7fc137b1e7f82857
Autor:
Vladimir Kaftan, M. V. Rodkin
Publikováno v:
Geodesy and Geodynamics, Vol 8, Iss 1, Pp 13-16 (2017)
We have examined the aftershock sequence and the post-seismic deformation process of the Parkfield earthquake (2004, M = 6, California, USA) source area using GPS data. This event was chosen because of the possibility of joint analysis of data from t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c415465bc159854ada03517abd2cc63c
https://doi.org/10.1016/j.geog.2017.01.001
https://doi.org/10.1016/j.geog.2017.01.001
Autor:
Normand, Raphaël
The Makran subduction zone of southeastern Iran has not experienced a megathrust earthquake in recent history, yet, the presence of uplifted coastal morphologies indicate that the margin is still tectonically active. In this work, we study three type
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::458c79dbbf885f9d5433c5da17503f54
Akademický článek
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Publikováno v:
Annals of Geophysics, Vol 53, Iss 2, Pp 89-99 (2010)
We performed an analysis of post-seismic stress relaxation, taking into account generalized linear rheologies. We compared the stress field (and its derived functions) obtained with a classical Maxwell rheology with that obtained with a transient Bur
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::153a45bd0f8e8dd31a50540915f0eac3
http://www.annalsofgeophysics.eu/index.php/annals/article/view/4642
http://www.annalsofgeophysics.eu/index.php/annals/article/view/4642
Publikováno v:
Geophysical Journal International. 153:645-657
SUMMARY An attempt at quantifying post-seismic relaxation triggered by decoupling earthquakes along the eastern thrusting border of the Adriatic plate (southern Dinarides) is carried out by finite element modelling, with a model constituted by an ela
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::adfa56f6f97bd1855e7fe7efef24d519
https://doi.org/10.1046/j.1365-246x.2003.01939.x
https://doi.org/10.1046/j.1365-246x.2003.01939.x
The strong earthquake ( M = 7) that occurred in the Fucino basin (central Italy) on January 13, 1915 was followed by six earthquakes of M > 5.5 and several other shocks of M > 5 in the major seismic zones of the northern Apennines from 1916 to 1920.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::5673677ee27117db8514f7354a0ce514
http://hdl.handle.net/11577/3317361
http://hdl.handle.net/11577/3317361