Is the dependence on the temperature of the friction important in stress triggering phenomena? The case of the 2000 Iceland seismic sequence ...

We perform numerical experiments by using a mass–spring fault model subject to an external coseismic stress perturbation due to a remote seismic event happening on another fault, the causative fault. In particular, the aim of this study is to investigate the instantaneous fault interaction and possi...

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Main Authors: Bizzarri, Andrea, Crupi, Paola, De Lorenzo, Salvatore, Loddo, Mariano
Format: Article in Journal/Newspaper
Language:English
Published: Istituto Nazionale di Geofisica e Vulcanologia (INGV) 2012
Subjects:
Online Access:https://dx.doi.org/10.13127/rpt/222
https://editoria.ingv.it/rapporti/2012/rapporto222/
id ftdatacite:10.13127/rpt/222
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spelling ftdatacite:10.13127/rpt/222 2024-06-09T07:46:59+00:00 Is the dependence on the temperature of the friction important in stress triggering phenomena? The case of the 2000 Iceland seismic sequence ... Bizzarri, Andrea Crupi, Paola De Lorenzo, Salvatore Loddo, Mariano 2012 application/pdf https://dx.doi.org/10.13127/rpt/222 https://editoria.ingv.it/rapporti/2012/rapporto222/ en eng Istituto Nazionale di Geofisica e Vulcanologia (INGV) Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 Text ScholarlyArticle JournalArticle article-journal 2012 ftdatacite https://doi.org/10.13127/rpt/222 2024-05-13T13:21:07Z We perform numerical experiments by using a mass–spring fault model subject to an external coseismic stress perturbation due to a remote seismic event happening on another fault, the causative fault. In particular, the aim of this study is to investigate the instantaneous fault interaction and possible triggering that happens when a fault perturbed by a stress change fails before the so–called unperturbed instability. As a realistic example we focus our attention on the instantaneous dynamic triggering phenomena occurred during the 17 June 2000 south Iceland seismic sequence in the South Iceland Seismic Zone (SISZ, Reykjanes Peninsula). The main event (Ms 6.6) was followed by three large events within a few tens of seconds (8, 26 and 30 s, respectively) located in a neighborhood of several tens of km. Among them the 26 s event was the best constrained (Bizzarri and Belardinelli, 2008). In the present study, conditions to simulate the instantaneous dynamic triggering connected to the former three events, have ... Article in Journal/Newspaper Iceland DataCite Metadata Store (German National Library of Science and Technology) Reykjanes ENVELOPE(-22.250,-22.250,65.467,65.467)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
description We perform numerical experiments by using a mass–spring fault model subject to an external coseismic stress perturbation due to a remote seismic event happening on another fault, the causative fault. In particular, the aim of this study is to investigate the instantaneous fault interaction and possible triggering that happens when a fault perturbed by a stress change fails before the so–called unperturbed instability. As a realistic example we focus our attention on the instantaneous dynamic triggering phenomena occurred during the 17 June 2000 south Iceland seismic sequence in the South Iceland Seismic Zone (SISZ, Reykjanes Peninsula). The main event (Ms 6.6) was followed by three large events within a few tens of seconds (8, 26 and 30 s, respectively) located in a neighborhood of several tens of km. Among them the 26 s event was the best constrained (Bizzarri and Belardinelli, 2008). In the present study, conditions to simulate the instantaneous dynamic triggering connected to the former three events, have ...
format Article in Journal/Newspaper
author Bizzarri, Andrea
Crupi, Paola
De Lorenzo, Salvatore
Loddo, Mariano
spellingShingle Bizzarri, Andrea
Crupi, Paola
De Lorenzo, Salvatore
Loddo, Mariano
Is the dependence on the temperature of the friction important in stress triggering phenomena? The case of the 2000 Iceland seismic sequence ...
author_facet Bizzarri, Andrea
Crupi, Paola
De Lorenzo, Salvatore
Loddo, Mariano
author_sort Bizzarri, Andrea
title Is the dependence on the temperature of the friction important in stress triggering phenomena? The case of the 2000 Iceland seismic sequence ...
title_short Is the dependence on the temperature of the friction important in stress triggering phenomena? The case of the 2000 Iceland seismic sequence ...
title_full Is the dependence on the temperature of the friction important in stress triggering phenomena? The case of the 2000 Iceland seismic sequence ...
title_fullStr Is the dependence on the temperature of the friction important in stress triggering phenomena? The case of the 2000 Iceland seismic sequence ...
title_full_unstemmed Is the dependence on the temperature of the friction important in stress triggering phenomena? The case of the 2000 Iceland seismic sequence ...
title_sort is the dependence on the temperature of the friction important in stress triggering phenomena? the case of the 2000 iceland seismic sequence ...
publisher Istituto Nazionale di Geofisica e Vulcanologia (INGV)
publishDate 2012
url https://dx.doi.org/10.13127/rpt/222
https://editoria.ingv.it/rapporti/2012/rapporto222/
long_lat ENVELOPE(-22.250,-22.250,65.467,65.467)
geographic Reykjanes
geographic_facet Reykjanes
genre Iceland
genre_facet Iceland
op_rights Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
op_doi https://doi.org/10.13127/rpt/222
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