Complex rupture of the M6.3 2015 March 10 Bucaramanga earthquake: evidence of strong weakening process
We use seismic waves for a magnitude 6.3 intermediate-depth (160?km) earthquake in the Bucaramanga Nest, Colombia, to infer a complex rupture process with two distinct stages, characterized by different rupture velocities possibly controlled by the evolution of strength on the fault. Our integrated...
- Autores:
- Tipo de recurso:
- Fecha de publicación:
- 2016
- Institución:
- Universidad del Rosario
- Repositorio:
- Repositorio EdocUR - U. Rosario
- Idioma:
- eng
- OAI Identifier:
- oai:repository.urosario.edu.co:10336/27400
- Acceso en línea:
- https://doi.org/10.1093/gji/ggw065
https://repository.urosario.edu.co/handle/10336/27400
- Palabra clave:
- Earthquake dynamics
Earthquake source observations
Body waves
- Rights
- License
- Abierto (Texto Completo)
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5afd3290-2cd3-4a38-8b6e-51e70c21bd9a-1bd8e04ca-9e29-4331-a4b8-c2121273d723-1af8cbac5-c134-4833-b18a-266e1037f833-1e7be3db0-14fb-4a19-8490-baba74635139-169eaf95d-5b53-4182-9687-e9dde06c1949-126a8af04-0e5e-49d0-8577-5b1759e308f7-1afe61638-7f0f-4cbc-b0fc-821933cd2d5f-1addcbeba-9f5c-4e07-9317-4f102ef275fc-1ae2ba17d-bf61-4a85-9448-0997529ec80a-12020-08-19T14:42:02Z2020-08-19T14:42:02Z2016-02-15We use seismic waves for a magnitude 6.3 intermediate-depth (160?km) earthquake in the Bucaramanga Nest, Colombia, to infer a complex rupture process with two distinct stages, characterized by different rupture velocities possibly controlled by the evolution of strength on the fault. Our integrated data processing permitted to precisely characterize the multistage rupture and the presence of a strong weakening event. The resulting seismic radiation is interpreted as resulting from an extreme weakening due to a cascading thermal shear runaway, with an initial inefficient radiation process followed by a fast and dynamic efficient rupture. Our results imply dynamic complexity of the seismic rupture deep inside the Earth, and may help to give some new insights about the physical mechanism of intermediate-depth earthquakes.application/pdfhttps://doi.org/10.1093/gji/ggw065ISSN: 0956-540XEISSN: 1365-246Xhttps://repository.urosario.edu.co/handle/10336/27400engThe Royal Astronomical SocietyOxford University Press994No. 2988Geophysical Journal InternationalVol. 205Geophysical Journal International, ISSN: 0956-540X;EISSN: 1365-246X, Vol.205, No.2 (01 May 2016); pp. 988–994https://academic.oup.com/gji/article/205/2/988/689612Abierto (Texto Completo)http://purl.org/coar/access_right/c_abf2Geophysical Journal Internationalinstname:Universidad del Rosarioreponame:Repositorio Institucional EdocUREarthquake dynamicsEarthquake source observationsBody wavesComplex rupture of the M6.3 2015 March 10 Bucaramanga earthquake: evidence of strong weakening processRuptura compleja del terremoto M6.3 del 10 de marzo de 2015 en Bucaramanga: evidencia de un fuerte proceso de debilitamientoarticleArtículohttp://purl.org/coar/version/c_970fb48d4fbd8a85http://purl.org/coar/resource_type/c_6501Poli, P.Prieto, G.A.Yu, C.Q.Florez, M.Agurto-Detzel, H.Mikesell, T.D.Chen, G.Dionicio, V.Pedraza, P.10336/27400oai:repository.urosario.edu.co:10336/274002021-06-03 00:50:12.194https://repository.urosario.edu.coRepositorio institucional EdocURedocur@urosario.edu.co |
dc.title.spa.fl_str_mv |
Complex rupture of the M6.3 2015 March 10 Bucaramanga earthquake: evidence of strong weakening process |
dc.title.TranslatedTitle.spa.fl_str_mv |
Ruptura compleja del terremoto M6.3 del 10 de marzo de 2015 en Bucaramanga: evidencia de un fuerte proceso de debilitamiento |
title |
Complex rupture of the M6.3 2015 March 10 Bucaramanga earthquake: evidence of strong weakening process |
spellingShingle |
Complex rupture of the M6.3 2015 March 10 Bucaramanga earthquake: evidence of strong weakening process Earthquake dynamics Earthquake source observations Body waves |
title_short |
Complex rupture of the M6.3 2015 March 10 Bucaramanga earthquake: evidence of strong weakening process |
title_full |
Complex rupture of the M6.3 2015 March 10 Bucaramanga earthquake: evidence of strong weakening process |
title_fullStr |
Complex rupture of the M6.3 2015 March 10 Bucaramanga earthquake: evidence of strong weakening process |
title_full_unstemmed |
Complex rupture of the M6.3 2015 March 10 Bucaramanga earthquake: evidence of strong weakening process |
title_sort |
Complex rupture of the M6.3 2015 March 10 Bucaramanga earthquake: evidence of strong weakening process |
dc.subject.keyword.spa.fl_str_mv |
Earthquake dynamics Earthquake source observations Body waves |
topic |
Earthquake dynamics Earthquake source observations Body waves |
description |
We use seismic waves for a magnitude 6.3 intermediate-depth (160?km) earthquake in the Bucaramanga Nest, Colombia, to infer a complex rupture process with two distinct stages, characterized by different rupture velocities possibly controlled by the evolution of strength on the fault. Our integrated data processing permitted to precisely characterize the multistage rupture and the presence of a strong weakening event. The resulting seismic radiation is interpreted as resulting from an extreme weakening due to a cascading thermal shear runaway, with an initial inefficient radiation process followed by a fast and dynamic efficient rupture. Our results imply dynamic complexity of the seismic rupture deep inside the Earth, and may help to give some new insights about the physical mechanism of intermediate-depth earthquakes. |
publishDate |
2016 |
dc.date.created.spa.fl_str_mv |
2016-02-15 |
dc.date.accessioned.none.fl_str_mv |
2020-08-19T14:42:02Z |
dc.date.available.none.fl_str_mv |
2020-08-19T14:42:02Z |
dc.type.eng.fl_str_mv |
article |
dc.type.coarversion.fl_str_mv |
http://purl.org/coar/version/c_970fb48d4fbd8a85 |
dc.type.coar.fl_str_mv |
http://purl.org/coar/resource_type/c_6501 |
dc.type.spa.spa.fl_str_mv |
Artículo |
dc.identifier.doi.none.fl_str_mv |
https://doi.org/10.1093/gji/ggw065 |
dc.identifier.issn.none.fl_str_mv |
ISSN: 0956-540X EISSN: 1365-246X |
dc.identifier.uri.none.fl_str_mv |
https://repository.urosario.edu.co/handle/10336/27400 |
url |
https://doi.org/10.1093/gji/ggw065 https://repository.urosario.edu.co/handle/10336/27400 |
identifier_str_mv |
ISSN: 0956-540X EISSN: 1365-246X |
dc.language.iso.spa.fl_str_mv |
eng |
language |
eng |
dc.relation.citationEndPage.none.fl_str_mv |
994 |
dc.relation.citationIssue.none.fl_str_mv |
No. 2 |
dc.relation.citationStartPage.none.fl_str_mv |
988 |
dc.relation.citationTitle.none.fl_str_mv |
Geophysical Journal International |
dc.relation.citationVolume.none.fl_str_mv |
Vol. 205 |
dc.relation.ispartof.spa.fl_str_mv |
Geophysical Journal International, ISSN: 0956-540X;EISSN: 1365-246X, Vol.205, No.2 (01 May 2016); pp. 988–994 |
dc.relation.uri.spa.fl_str_mv |
https://academic.oup.com/gji/article/205/2/988/689612 |
dc.rights.coar.fl_str_mv |
http://purl.org/coar/access_right/c_abf2 |
dc.rights.acceso.spa.fl_str_mv |
Abierto (Texto Completo) |
rights_invalid_str_mv |
Abierto (Texto Completo) http://purl.org/coar/access_right/c_abf2 |
dc.format.mimetype.none.fl_str_mv |
application/pdf |
dc.publisher.spa.fl_str_mv |
The Royal Astronomical Society Oxford University Press |
dc.source.spa.fl_str_mv |
Geophysical Journal International |
institution |
Universidad del Rosario |
dc.source.instname.none.fl_str_mv |
instname:Universidad del Rosario |
dc.source.reponame.none.fl_str_mv |
reponame:Repositorio Institucional EdocUR |
repository.name.fl_str_mv |
Repositorio institucional EdocUR |
repository.mail.fl_str_mv |
edocur@urosario.edu.co |
_version_ |
1814167696768499712 |