Sismotectonics and geodynamics characterization of Murindo - Colombia seismic source

Northwestern South America is a convergence zone of three major tectonic plates, Nazca, Caribbean and South America and microplates or blocks such as Panama-Costa Rica, Choco and the Northern Andean or Macondo. The displacement of these plates and microplates produce seismotectonic stresses, which h...

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Tipo de recurso:
Fecha de publicación:
2005
Institución:
Universidad Industrial de Santander
Repositorio:
Repositorio UIS
Idioma:
spa
OAI Identifier:
oai:noesis.uis.edu.co:20.500.14071/5011
Acceso en línea:
https://revistas.uis.edu.co/index.php/revistaboletindegeologia/article/view/863
https://noesis.uis.edu.co/handle/20.500.14071/5011
Palabra clave:
Seismotectonic
geodynamics
focal mechanisms solutions
strain rate
Murindó Zone
GPS
sismotectónica
geodinámica
mecanismos focales
velocidad de deformación
Zona de Murindó
GPS
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openAccess
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Attribution-NonCommercial 4.0 International (CC BY-NC 4.0)
id UISANTADR2_8e74e28e8cd77ea49111b782841a646e
oai_identifier_str oai:noesis.uis.edu.co:20.500.14071/5011
network_acronym_str UISANTADR2
network_name_str Repositorio UIS
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spelling Attribution-NonCommercial 4.0 International (CC BY-NC 4.0)http://purl.org/coar/access_right/c_abf2info:eu-repo/semantics/openAccessAtribución-NoComercial-SinDerivadas 4.0 Internacional (CC BY-NC-ND 4.0)2005-01-112022-03-14T20:07:55Z2022-03-14T20:07:55Zhttps://revistas.uis.edu.co/index.php/revistaboletindegeologia/article/view/863https://noesis.uis.edu.co/handle/20.500.14071/5011Northwestern South America is a convergence zone of three major tectonic plates, Nazca, Caribbean and South America and microplates or blocks such as Panama-Costa Rica, Choco and the Northern Andean or Macondo. The displacement of these plates and microplates produce seismotectonic stresses, which have generated strong earthquakes when release. The seismic events occurred in this zone are shallow focus and destructive, reaching up to Ms = 7.5. Using empirical mathematical relationships with magnitude Ms ≥ 3,9, focal mechanism solutions and GPS plate tectonic displacement vectors, the seismotectonic deformation was analyzed. This deformation is represented by the North component of the seismic moment tensor. Low deformation velocity was obtained, which is in contrast with those determined by GPS. Therefore, we proposed that the regional stresses do not behave homogeneously on the zone.  La esquina noroccidental de Suramérica es una zona de convergencia de tres placas tectónicas principales, Nazca, Caribe y Suramericana, Acosta, J. (2000). Structure, tectonics and 3D Models of the Western foothills of the Eastern Cordillera and Middle Magdalena Valley , Colombia. Publicación Especial N° 25, Ingeominas acondo. El movimiento de estas placas y microplacas generan esfuerzos deformantes que al liberarse, causan sismos fuertes. Los sismos ocurridos en esta zona son superficiales y destructores, y de acuerdo con los cálculos podrían alcanzar magnitudes Ms hasta de 7,5. El análisis de la deformación producida por estos eventos fue determinada a partir de relaciones matemáticas empíricas utilizando datos de magnitud Ms ≥ 3,9, solución de mecanismos focales, y datos de mediciones realizadas con geodesia satelital GPS (Sistema de Posicionamiento Global). La deformación sismotectónica predominante se especifica por la componente del tensor de momento sísmico en sentido norte. Las velocidades de deformación obtenidas a partir de datos sismológicos son muy bajas, a diferencia de las obtenidas por GPS, lo cual muestra que los esfuerzos regionales no actúan de forma homogénea en la zona.  application/pdfspaUniversidad Industrial de Santanderhttps://revistas.uis.edu.co/index.php/revistaboletindegeologia/article/view/863/1192Boletín de Geología; Vol. 27 Núm. 1 (2005): Boletin de Geología; 115-132Boletín de Geología; Vol. 27 No. 1 (2005): Boletin de Geología; 115-132BOLETÍN DE GEOLOGÍA; v. 27 n. 1 (2005): Boletin de Geología; 115-1322145-85530120-0283Seismotectonicgeodynamicsfocal mechanisms solutionsstrain rateMurindó ZoneGPSsismotectónicageodinámicamecanismos focalesvelocidad de deformaciónZona de MurindóGPSSismotectonics and geodynamics characterization of Murindo - Colombia seismic sourceCaracterización sismotectónica y geodinámica de la fuente sismogénica de Murindó - Colombiainfo:eu-repo/semantics/articlehttp://purl.org/coar/version/c_970fb48d4fbd8a85http://purl.org/coar/resource_type/c_2df8fbb1Cardona, C.Salcedo, E. de J.Mora, H.20.500.14071/5011oai:noesis.uis.edu.co:20.500.14071/50112022-03-16 12:39:34.158metadata.onlyhttps://noesis.uis.edu.coDSpace at UISnoesis@uis.edu.co
dc.title.en-US.fl_str_mv Sismotectonics and geodynamics characterization of Murindo - Colombia seismic source
dc.title.es-ES.fl_str_mv Caracterización sismotectónica y geodinámica de la fuente sismogénica de Murindó - Colombia
title Sismotectonics and geodynamics characterization of Murindo - Colombia seismic source
spellingShingle Sismotectonics and geodynamics characterization of Murindo - Colombia seismic source
Seismotectonic
geodynamics
focal mechanisms solutions
strain rate
Murindó Zone
GPS
sismotectónica
geodinámica
mecanismos focales
velocidad de deformación
Zona de Murindó
GPS
title_short Sismotectonics and geodynamics characterization of Murindo - Colombia seismic source
title_full Sismotectonics and geodynamics characterization of Murindo - Colombia seismic source
title_fullStr Sismotectonics and geodynamics characterization of Murindo - Colombia seismic source
title_full_unstemmed Sismotectonics and geodynamics characterization of Murindo - Colombia seismic source
title_sort Sismotectonics and geodynamics characterization of Murindo - Colombia seismic source
dc.subject.en-US.fl_str_mv Seismotectonic
geodynamics
focal mechanisms solutions
strain rate
Murindó Zone
GPS
topic Seismotectonic
geodynamics
focal mechanisms solutions
strain rate
Murindó Zone
GPS
sismotectónica
geodinámica
mecanismos focales
velocidad de deformación
Zona de Murindó
GPS
dc.subject.es-ES.fl_str_mv sismotectónica
geodinámica
mecanismos focales
velocidad de deformación
Zona de Murindó
GPS
description Northwestern South America is a convergence zone of three major tectonic plates, Nazca, Caribbean and South America and microplates or blocks such as Panama-Costa Rica, Choco and the Northern Andean or Macondo. The displacement of these plates and microplates produce seismotectonic stresses, which have generated strong earthquakes when release. The seismic events occurred in this zone are shallow focus and destructive, reaching up to Ms = 7.5. Using empirical mathematical relationships with magnitude Ms ≥ 3,9, focal mechanism solutions and GPS plate tectonic displacement vectors, the seismotectonic deformation was analyzed. This deformation is represented by the North component of the seismic moment tensor. Low deformation velocity was obtained, which is in contrast with those determined by GPS. Therefore, we proposed that the regional stresses do not behave homogeneously on the zone.
publishDate 2005
dc.date.accessioned.none.fl_str_mv 2022-03-14T20:07:55Z
dc.date.available.none.fl_str_mv 2022-03-14T20:07:55Z
dc.date.none.fl_str_mv 2005-01-11
dc.type.none.fl_str_mv info:eu-repo/semantics/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_2df8fbb1
dc.identifier.none.fl_str_mv https://revistas.uis.edu.co/index.php/revistaboletindegeologia/article/view/863
dc.identifier.uri.none.fl_str_mv https://noesis.uis.edu.co/handle/20.500.14071/5011
url https://revistas.uis.edu.co/index.php/revistaboletindegeologia/article/view/863
https://noesis.uis.edu.co/handle/20.500.14071/5011
dc.language.none.fl_str_mv spa
language spa
dc.relation.none.fl_str_mv https://revistas.uis.edu.co/index.php/revistaboletindegeologia/article/view/863/1192
dc.rights.license.none.fl_str_mv Attribution-NonCommercial 4.0 International (CC BY-NC 4.0)
dc.rights.coar.none.fl_str_mv http://purl.org/coar/access_right/c_abf2
dc.rights.accessrights.none.fl_str_mv info:eu-repo/semantics/openAccess
dc.rights.creativecommons.none.fl_str_mv Atribución-NoComercial-SinDerivadas 4.0 Internacional (CC BY-NC-ND 4.0)
rights_invalid_str_mv Attribution-NonCommercial 4.0 International (CC BY-NC 4.0)
http://purl.org/coar/access_right/c_abf2
Atribución-NoComercial-SinDerivadas 4.0 Internacional (CC BY-NC-ND 4.0)
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv application/pdf
dc.publisher.es-ES.fl_str_mv Universidad Industrial de Santander
dc.source.es-ES.fl_str_mv Boletín de Geología; Vol. 27 Núm. 1 (2005): Boletin de Geología; 115-132
dc.source.en-US.fl_str_mv Boletín de Geología; Vol. 27 No. 1 (2005): Boletin de Geología; 115-132
dc.source.pt-BR.fl_str_mv BOLETÍN DE GEOLOGÍA; v. 27 n. 1 (2005): Boletin de Geología; 115-132
dc.source.none.fl_str_mv 2145-8553
0120-0283
institution Universidad Industrial de Santander
repository.name.fl_str_mv DSpace at UIS
repository.mail.fl_str_mv noesis@uis.edu.co
_version_ 1814095206037848064

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