A successfully stress-forecast earthquake
A M = 5 earthquake in Iceland has been successfully ‘stress forecast’ by using variations in time delays of seismic shear wave splitting to assess the time and magnitude at which stress-modified microcracking reaches fracture criticality within the stressed volume where strain is released. Local inv...
Published in: | Geophysical Journal International |
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Oxford University Press
1999
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fthighwire:oai:open-archive.highwire.org:gji:138/1/F1 2023-05-15T16:47:27+02:00 A successfully stress-forecast earthquake Crampin, Stuart Volti, Theodora Stefánsson, Ragnar 1999-07-01 00:00:00.0 text/html http://gji.oxfordjournals.org/cgi/content/short/138/1/F1 https://doi.org/10.1046/j.1365-246x.1999.00891.x en eng Oxford University Press http://gji.oxfordjournals.org/cgi/content/short/138/1/F1 http://dx.doi.org/10.1046/j.1365-246x.1999.00891.x Copyright (C) 1999, Oxford University Press Fast-Track Paper TEXT 1999 fthighwire https://doi.org/10.1046/j.1365-246x.1999.00891.x 2015-02-28T21:10:35Z A M = 5 earthquake in Iceland has been successfully ‘stress forecast’ by using variations in time delays of seismic shear wave splitting to assess the time and magnitude at which stress-modified microcracking reaches fracture criticality within the stressed volume where strain is released. Local investigations suggested the approximate location of the forecast earthquake. We report the criteria on which this stress forecast was based. Text Iceland HighWire Press (Stanford University) Geophysical Journal International 138 1 F1 F5 |
institution |
Open Polar |
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HighWire Press (Stanford University) |
op_collection_id |
fthighwire |
language |
English |
topic |
Fast-Track Paper |
spellingShingle |
Fast-Track Paper Crampin, Stuart Volti, Theodora Stefánsson, Ragnar A successfully stress-forecast earthquake |
topic_facet |
Fast-Track Paper |
description |
A M = 5 earthquake in Iceland has been successfully ‘stress forecast’ by using variations in time delays of seismic shear wave splitting to assess the time and magnitude at which stress-modified microcracking reaches fracture criticality within the stressed volume where strain is released. Local investigations suggested the approximate location of the forecast earthquake. We report the criteria on which this stress forecast was based. |
format |
Text |
author |
Crampin, Stuart Volti, Theodora Stefánsson, Ragnar |
author_facet |
Crampin, Stuart Volti, Theodora Stefánsson, Ragnar |
author_sort |
Crampin, Stuart |
title |
A successfully stress-forecast earthquake |
title_short |
A successfully stress-forecast earthquake |
title_full |
A successfully stress-forecast earthquake |
title_fullStr |
A successfully stress-forecast earthquake |
title_full_unstemmed |
A successfully stress-forecast earthquake |
title_sort |
successfully stress-forecast earthquake |
publisher |
Oxford University Press |
publishDate |
1999 |
url |
http://gji.oxfordjournals.org/cgi/content/short/138/1/F1 https://doi.org/10.1046/j.1365-246x.1999.00891.x |
genre |
Iceland |
genre_facet |
Iceland |
op_relation |
http://gji.oxfordjournals.org/cgi/content/short/138/1/F1 http://dx.doi.org/10.1046/j.1365-246x.1999.00891.x |
op_rights |
Copyright (C) 1999, Oxford University Press |
op_doi |
https://doi.org/10.1046/j.1365-246x.1999.00891.x |
container_title |
Geophysical Journal International |
container_volume |
138 |
container_issue |
1 |
container_start_page |
F1 |
op_container_end_page |
F5 |
_version_ |
1766037543283851264 |