Seismic source characteristics of the intraslab 2017 Chiapas-Mexico earthquake (Mw8.2)
Descripción del Articulo
This research was sponsored in part by the Vice-rectorate for Research and Postgraduate from “Universidad Nacional Mayor de San Marcos”, by CONCYTEC through the Teacher-Researcher bonus and by the “Direccion de Hidrografia y Navegacion” from the Peruvian Navy. In addition, we acknowledge the anonymo...
| Autor: | |
|---|---|
| Formato: | artículo |
| Fecha de Publicación: | 2018 |
| Institución: | Consejo Nacional de Ciencia Tecnología e Innovación |
| Repositorio: | CONCYTEC-Institucional |
| Lenguaje: | inglés |
| OAI Identifier: | oai:repositorio.concytec.gob.pe:20.500.12390/595 |
| Enlace del recurso: | https://hdl.handle.net/20.500.12390/595 https://doi.org/10.1016/j.pepi.2018.04.013 |
| Nivel de acceso: | acceso abierto |
| Materia: | Unidirectional propagation Faulting Seismic waves Shear waves Deformation pattern Epicentral distances Finite fault inversions Inversion Mexico earthquake Moment magnitudes Seismic source Earthquakes earthquake epicenter earthquake event earthquake magnitude earthquake rupture fault plane focal mechanism normal fault seismic data seismic source Chiapas Mexico [North America] https://purl.org/pe-repo/ocde/ford#1.05.06 |
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| dc.title.none.fl_str_mv |
Seismic source characteristics of the intraslab 2017 Chiapas-Mexico earthquake (Mw8.2) |
| title |
Seismic source characteristics of the intraslab 2017 Chiapas-Mexico earthquake (Mw8.2) |
| spellingShingle |
Seismic source characteristics of the intraslab 2017 Chiapas-Mexico earthquake (Mw8.2) Jiménez C. Unidirectional propagation Faulting Seismic waves Shear waves Deformation pattern Epicentral distances Finite fault inversions Inversion Mexico earthquake Moment magnitudes Seismic source Earthquakes earthquake epicenter earthquake event earthquake magnitude earthquake rupture fault plane focal mechanism normal fault seismic data seismic source Chiapas Mexico [North America] https://purl.org/pe-repo/ocde/ford#1.05.06 |
| title_short |
Seismic source characteristics of the intraslab 2017 Chiapas-Mexico earthquake (Mw8.2) |
| title_full |
Seismic source characteristics of the intraslab 2017 Chiapas-Mexico earthquake (Mw8.2) |
| title_fullStr |
Seismic source characteristics of the intraslab 2017 Chiapas-Mexico earthquake (Mw8.2) |
| title_full_unstemmed |
Seismic source characteristics of the intraslab 2017 Chiapas-Mexico earthquake (Mw8.2) |
| title_sort |
Seismic source characteristics of the intraslab 2017 Chiapas-Mexico earthquake (Mw8.2) |
| author |
Jiménez C. |
| author_facet |
Jiménez C. |
| author_role |
author |
| dc.contributor.author.fl_str_mv |
Jiménez C. |
| dc.subject.none.fl_str_mv |
Unidirectional propagation |
| topic |
Unidirectional propagation Faulting Seismic waves Shear waves Deformation pattern Epicentral distances Finite fault inversions Inversion Mexico earthquake Moment magnitudes Seismic source Earthquakes earthquake epicenter earthquake event earthquake magnitude earthquake rupture fault plane focal mechanism normal fault seismic data seismic source Chiapas Mexico [North America] https://purl.org/pe-repo/ocde/ford#1.05.06 |
| dc.subject.es_PE.fl_str_mv |
Faulting Seismic waves Shear waves Deformation pattern Epicentral distances Finite fault inversions Inversion Mexico earthquake Moment magnitudes Seismic source Earthquakes earthquake epicenter earthquake event earthquake magnitude earthquake rupture fault plane focal mechanism normal fault seismic data seismic source Chiapas Mexico [North America] |
| dc.subject.ocde.none.fl_str_mv |
https://purl.org/pe-repo/ocde/ford#1.05.06 |
| description |
This research was sponsored in part by the Vice-rectorate for Research and Postgraduate from “Universidad Nacional Mayor de San Marcos”, by CONCYTEC through the Teacher-Researcher bonus and by the “Direccion de Hidrografia y Navegacion” from the Peruvian Navy. In addition, we acknowledge the anonymous reviewers for their valuable comments and observations. |
| publishDate |
2018 |
| dc.date.accessioned.none.fl_str_mv |
2024-05-30T23:13:38Z |
| dc.date.available.none.fl_str_mv |
2024-05-30T23:13:38Z |
| dc.date.issued.fl_str_mv |
2018 |
| dc.type.none.fl_str_mv |
info:eu-repo/semantics/article |
| format |
article |
| dc.identifier.uri.none.fl_str_mv |
https://hdl.handle.net/20.500.12390/595 |
| dc.identifier.doi.none.fl_str_mv |
https://doi.org/10.1016/j.pepi.2018.04.013 |
| dc.identifier.scopus.none.fl_str_mv |
2-s2.0-85047249035 |
| url |
https://hdl.handle.net/20.500.12390/595 https://doi.org/10.1016/j.pepi.2018.04.013 |
| identifier_str_mv |
2-s2.0-85047249035 |
| dc.language.iso.none.fl_str_mv |
eng |
| language |
eng |
| dc.relation.ispartof.none.fl_str_mv |
Physics of the Earth and Planetary Interiors |
| dc.rights.none.fl_str_mv |
info:eu-repo/semantics/openAccess |
| eu_rights_str_mv |
openAccess |
| dc.publisher.none.fl_str_mv |
Elsevier |
| publisher.none.fl_str_mv |
Elsevier |
| dc.source.none.fl_str_mv |
reponame:CONCYTEC-Institucional instname:Consejo Nacional de Ciencia Tecnología e Innovación instacron:CONCYTEC |
| instname_str |
Consejo Nacional de Ciencia Tecnología e Innovación |
| instacron_str |
CONCYTEC |
| institution |
CONCYTEC |
| reponame_str |
CONCYTEC-Institucional |
| collection |
CONCYTEC-Institucional |
| repository.name.fl_str_mv |
Repositorio Institucional CONCYTEC |
| repository.mail.fl_str_mv |
repositorio@concytec.gob.pe |
| _version_ |
1844882996692254720 |
| spelling |
Publicationrp01180600Jiménez C.2024-05-30T23:13:38Z2024-05-30T23:13:38Z2018https://hdl.handle.net/20.500.12390/595https://doi.org/10.1016/j.pepi.2018.04.0132-s2.0-85047249035This research was sponsored in part by the Vice-rectorate for Research and Postgraduate from “Universidad Nacional Mayor de San Marcos”, by CONCYTEC through the Teacher-Researcher bonus and by the “Direccion de Hidrografia y Navegacion” from the Peruvian Navy. In addition, we acknowledge the anonymous reviewers for their valuable comments and observations.Inversion of the parameters characterising the seismic source of the instraslab 2017 Chiapas Mexico earthquake (Mw 8.2) shows a simple rupture process with a unidirectional propagation and directivity towards the North-West and a duration of the rupture process around 75 s. The initial point source values of strike, dip and rake are 316°, 80° and −91° respectively. The focal mechanism indicates a normal fault type within the oceanic Cocos plate, with an almost vertical fault plane for a focal depth of 59 km. The seismic data was obtained from 51 seismic stations of the global seismic network IRIS for the epicentral distances between 30° and 90°. In the finite-fault inversion, 75 seismic signals between P and SH waves were used. The epicenter is on the southeast margin of the large slip zone which extends 75 km to the northwest, this large slip zone is located to the south of the city of Arriaga. The scalar seismic moment was estimated at , equivalent to a moment magnitude of Mw 8.2. The maximum dislocation or slip is 14.5 m. As a coseismic effect, a local tsunami was generated, recorded by several tidal gauges and offshore buoys. The deformation pattern shows a coastal uplift and subsidence.Consejo Nacional de Ciencia, Tecnología e Innovación Tecnológica - ConcytecengElsevierPhysics of the Earth and Planetary Interiorsinfo:eu-repo/semantics/openAccessUnidirectional propagationFaulting-1Seismic waves-1Shear waves-1Deformation pattern-1Epicentral distances-1Finite fault inversions-1Inversion-1Mexico earthquake-1Moment magnitudes-1Seismic source-1Earthquakes-1earthquake epicenter-1earthquake event-1earthquake magnitude-1earthquake rupture-1fault plane-1focal mechanism-1normal fault-1seismic data-1seismic source-1Chiapas-1Mexico [North America]-1https://purl.org/pe-repo/ocde/ford#1.05.06-1Seismic source characteristics of the intraslab 2017 Chiapas-Mexico earthquake (Mw8.2)info:eu-repo/semantics/articlereponame:CONCYTEC-Institucionalinstname:Consejo Nacional de Ciencia Tecnología e Innovacióninstacron:CONCYTEC20.500.12390/595oai:repositorio.concytec.gob.pe:20.500.12390/5952024-05-30 15:58:11.152http://purl.org/coar/access_right/c_14cbinfo:eu-repo/semantics/closedAccessmetadata only accesshttps://repositorio.concytec.gob.peRepositorio Institucional CONCYTECrepositorio@concytec.gob.pe#PLACEHOLDER_PARENT_METADATA_VALUE#<Publication xmlns="https://www.openaire.eu/cerif-profile/1.1/" id="8a9cbf2c-fa01-437e-974e-1018ee20bb73"> <Type xmlns="https://www.openaire.eu/cerif-profile/vocab/COAR_Publication_Types">http://purl.org/coar/resource_type/c_1843</Type> <Language>eng</Language> <Title>Seismic source characteristics of the intraslab 2017 Chiapas-Mexico earthquake (Mw8.2)</Title> <PublishedIn> <Publication> <Title>Physics of the Earth and Planetary Interiors</Title> </Publication> </PublishedIn> <PublicationDate>2018</PublicationDate> <DOI>https://doi.org/10.1016/j.pepi.2018.04.013</DOI> <SCP-Number>2-s2.0-85047249035</SCP-Number> <Authors> <Author> <DisplayName>Jiménez C.</DisplayName> <Person id="rp01180" /> <Affiliation> <OrgUnit> </OrgUnit> </Affiliation> </Author> </Authors> <Editors> </Editors> <Publishers> <Publisher> <DisplayName>Elsevier</DisplayName> <OrgUnit /> </Publisher> </Publishers> <Keyword>Unidirectional propagation</Keyword> <Keyword>Faulting</Keyword> <Keyword>Seismic waves</Keyword> <Keyword>Shear waves</Keyword> <Keyword>Deformation pattern</Keyword> <Keyword>Epicentral distances</Keyword> <Keyword>Finite fault inversions</Keyword> <Keyword>Inversion</Keyword> <Keyword>Mexico earthquake</Keyword> <Keyword>Moment magnitudes</Keyword> <Keyword>Seismic source</Keyword> <Keyword>Earthquakes</Keyword> <Keyword>earthquake epicenter</Keyword> <Keyword>earthquake event</Keyword> <Keyword>earthquake magnitude</Keyword> <Keyword>earthquake rupture</Keyword> <Keyword>fault plane</Keyword> <Keyword>focal mechanism</Keyword> <Keyword>normal fault</Keyword> <Keyword>seismic data</Keyword> <Keyword>seismic source</Keyword> <Keyword>Chiapas</Keyword> <Keyword>Mexico [North America]</Keyword> <Abstract>Inversion of the parameters characterising the seismic source of the instraslab 2017 Chiapas Mexico earthquake (Mw 8.2) shows a simple rupture process with a unidirectional propagation and directivity towards the North-West and a duration of the rupture process around 75 s. The initial point source values of strike, dip and rake are 316°, 80° and −91° respectively. The focal mechanism indicates a normal fault type within the oceanic Cocos plate, with an almost vertical fault plane for a focal depth of 59 km. The seismic data was obtained from 51 seismic stations of the global seismic network IRIS for the epicentral distances between 30° and 90°. In the finite-fault inversion, 75 seismic signals between P and SH waves were used. The epicenter is on the southeast margin of the large slip zone which extends 75 km to the northwest, this large slip zone is located to the south of the city of Arriaga. The scalar seismic moment was estimated at , equivalent to a moment magnitude of Mw 8.2. The maximum dislocation or slip is 14.5 m. As a coseismic effect, a local tsunami was generated, recorded by several tidal gauges and offshore buoys. The deformation pattern shows a coastal uplift and subsidence.</Abstract> <Access xmlns="http://purl.org/coar/access_right" > </Access> </Publication> -1 |
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13.457506 |
Nota importante:
La información contenida en este registro es de entera responsabilidad de la institución que gestiona el repositorio institucional donde esta contenido este documento o set de datos. El CONCYTEC no se hace responsable por los contenidos (publicaciones y/o datos) accesibles a través del Repositorio Nacional Digital de Ciencia, Tecnología e Innovación de Acceso Abierto (ALICIA).
La información contenida en este registro es de entera responsabilidad de la institución que gestiona el repositorio institucional donde esta contenido este documento o set de datos. El CONCYTEC no se hace responsable por los contenidos (publicaciones y/o datos) accesibles a través del Repositorio Nacional Digital de Ciencia, Tecnología e Innovación de Acceso Abierto (ALICIA).
