Evidencing Fluid Migration of the Crust during the Seismic Swarm by Using 1D Magnetotelluric Monitoring

Autores
Vargas, Carlos A.; Caneva, Alexander; Solano, Juan M.; Gulisano, Adriana Maria; Villalobos, Jaime
Año de publicación
2023
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
We applied multi–temporal 1D magnetotelluric (MT) surveys to identify space–time anomalies of apparent resistivity ((Formula presented.)) in the upper lithosphere in the Antarctic Peninsula (the border between the Antarctic and the Shetland plates). We used time series over several weeks of the natural Earth’s electric and magnetic fields registered at one MT station of the Universidad Nacional de Colombia (RSUNAL) located at Seymour–Marambio Island, Antarctica. We associated resistivity anomalies with contrasting earthquake activity. Anomalies of (Formula presented.) were detected almost simultaneously with the beginning of a seismic crisis in the Bransfield Strait, south of King George Island (approximately 85.000 events were reported close to the Orca submarine volcano, with focal depths < 20 km and MWW < 6.9). We explained the origin of these anomalies in response to fluid migration near the place of the fractures linked with the seismic swarm, which could promote disturbances of the pore pressure field that reached some hundreds of km away.
Fil: Vargas, Carlos A.. Universidad Nacional de Colombia; Colombia
Fil: Caneva, Alexander. Universidad Nacional de Colombia; Colombia
Fil: Solano, Juan M.. Universidad Nacional de Colombia; Colombia
Fil: Gulisano, Adriana Maria. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Astronomía y Física del Espacio. - Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Astronomía y Física del Espacio; Argentina. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Departamento de Física; Argentina. Ministerio de Relaciones Exteriores, Comercio Interno y Culto. Dirección Nacional del Antártico. Instituto Antártico Argentino; Argentina
Fil: Villalobos, Jaime. Universidad Nacional de Colombia; Colombia
Materia
ANTARCTIC PENINSULA
APPARENT RESISTIVITY
EARTHQUAKES
ELECTROMAGNETIC ANOMALIES
MAGNETOTELLURICS
ORCA SUBMARINE VOLCANO
SEYMOUR–MARAMBIO ISLAND
Nivel de accesibilidad
acceso abierto
Condiciones de uso
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
Repositorio
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/219722
Acceder
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network_acronym_str CONICETDig
repository_id_str 3498
network_name_str CONICET Digital (CONICET)
spelling Evidencing Fluid Migration of the Crust during the Seismic Swarm by Using 1D Magnetotelluric MonitoringVargas, Carlos A.Caneva, AlexanderSolano, Juan M.Gulisano, Adriana MariaVillalobos, JaimeANTARCTIC PENINSULAAPPARENT RESISTIVITYEARTHQUAKESELECTROMAGNETIC ANOMALIESMAGNETOTELLURICSORCA SUBMARINE VOLCANOSEYMOUR–MARAMBIO ISLANDhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1We applied multi–temporal 1D magnetotelluric (MT) surveys to identify space–time anomalies of apparent resistivity ((Formula presented.)) in the upper lithosphere in the Antarctic Peninsula (the border between the Antarctic and the Shetland plates). We used time series over several weeks of the natural Earth’s electric and magnetic fields registered at one MT station of the Universidad Nacional de Colombia (RSUNAL) located at Seymour–Marambio Island, Antarctica. We associated resistivity anomalies with contrasting earthquake activity. Anomalies of (Formula presented.) were detected almost simultaneously with the beginning of a seismic crisis in the Bransfield Strait, south of King George Island (approximately 85.000 events were reported close to the Orca submarine volcano, with focal depths < 20 km and MWW < 6.9). We explained the origin of these anomalies in response to fluid migration near the place of the fractures linked with the seismic swarm, which could promote disturbances of the pore pressure field that reached some hundreds of km away.Fil: Vargas, Carlos A.. Universidad Nacional de Colombia; ColombiaFil: Caneva, Alexander. Universidad Nacional de Colombia; ColombiaFil: Solano, Juan M.. Universidad Nacional de Colombia; ColombiaFil: Gulisano, Adriana Maria. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Astronomía y Física del Espacio. - Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Astronomía y Física del Espacio; Argentina. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Departamento de Física; Argentina. Ministerio de Relaciones Exteriores, Comercio Interno y Culto. Dirección Nacional del Antártico. Instituto Antártico Argentino; ArgentinaFil: Villalobos, Jaime. Universidad Nacional de Colombia; ColombiaMDPI2023-02info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/219722Vargas, Carlos A.; Caneva, Alexander; Solano, Juan M.; Gulisano, Adriana Maria; Villalobos, Jaime; Evidencing Fluid Migration of the Crust during the Seismic Swarm by Using 1D Magnetotelluric Monitoring; MDPI; Applied Sciences; 13; 4; 2-2023; 1-122076-3417CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/https://doi.org/10.3390/app13042683info:eu-repo/semantics/altIdentifier/doi/10.3390/app13042683info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-29T10:37:48Zoai:ri.conicet.gov.ar:11336/219722instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982025-09-29 10:37:49.203CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Evidencing Fluid Migration of the Crust during the Seismic Swarm by Using 1D Magnetotelluric Monitoring
title Evidencing Fluid Migration of the Crust during the Seismic Swarm by Using 1D Magnetotelluric Monitoring
spellingShingle Evidencing Fluid Migration of the Crust during the Seismic Swarm by Using 1D Magnetotelluric Monitoring
Vargas, Carlos A.
ANTARCTIC PENINSULA
APPARENT RESISTIVITY
EARTHQUAKES
ELECTROMAGNETIC ANOMALIES
MAGNETOTELLURICS
ORCA SUBMARINE VOLCANO
SEYMOUR–MARAMBIO ISLAND
title_short Evidencing Fluid Migration of the Crust during the Seismic Swarm by Using 1D Magnetotelluric Monitoring
title_full Evidencing Fluid Migration of the Crust during the Seismic Swarm by Using 1D Magnetotelluric Monitoring
title_fullStr Evidencing Fluid Migration of the Crust during the Seismic Swarm by Using 1D Magnetotelluric Monitoring
title_full_unstemmed Evidencing Fluid Migration of the Crust during the Seismic Swarm by Using 1D Magnetotelluric Monitoring
title_sort Evidencing Fluid Migration of the Crust during the Seismic Swarm by Using 1D Magnetotelluric Monitoring
dc.creator.none.fl_str_mv Vargas, Carlos A.
Caneva, Alexander
Solano, Juan M.
Gulisano, Adriana Maria
Villalobos, Jaime
author Vargas, Carlos A.
author_facet Vargas, Carlos A.
Caneva, Alexander
Solano, Juan M.
Gulisano, Adriana Maria
Villalobos, Jaime
author_role author
author2 Caneva, Alexander
Solano, Juan M.
Gulisano, Adriana Maria
Villalobos, Jaime
author2_role author
author
author
author
dc.subject.none.fl_str_mv ANTARCTIC PENINSULA
APPARENT RESISTIVITY
EARTHQUAKES
ELECTROMAGNETIC ANOMALIES
MAGNETOTELLURICS
ORCA SUBMARINE VOLCANO
SEYMOUR–MARAMBIO ISLAND
topic ANTARCTIC PENINSULA
APPARENT RESISTIVITY
EARTHQUAKES
ELECTROMAGNETIC ANOMALIES
MAGNETOTELLURICS
ORCA SUBMARINE VOLCANO
SEYMOUR–MARAMBIO ISLAND
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv We applied multi–temporal 1D magnetotelluric (MT) surveys to identify space–time anomalies of apparent resistivity ((Formula presented.)) in the upper lithosphere in the Antarctic Peninsula (the border between the Antarctic and the Shetland plates). We used time series over several weeks of the natural Earth’s electric and magnetic fields registered at one MT station of the Universidad Nacional de Colombia (RSUNAL) located at Seymour–Marambio Island, Antarctica. We associated resistivity anomalies with contrasting earthquake activity. Anomalies of (Formula presented.) were detected almost simultaneously with the beginning of a seismic crisis in the Bransfield Strait, south of King George Island (approximately 85.000 events were reported close to the Orca submarine volcano, with focal depths < 20 km and MWW < 6.9). We explained the origin of these anomalies in response to fluid migration near the place of the fractures linked with the seismic swarm, which could promote disturbances of the pore pressure field that reached some hundreds of km away.
Fil: Vargas, Carlos A.. Universidad Nacional de Colombia; Colombia
Fil: Caneva, Alexander. Universidad Nacional de Colombia; Colombia
Fil: Solano, Juan M.. Universidad Nacional de Colombia; Colombia
Fil: Gulisano, Adriana Maria. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Astronomía y Física del Espacio. - Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Astronomía y Física del Espacio; Argentina. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Departamento de Física; Argentina. Ministerio de Relaciones Exteriores, Comercio Interno y Culto. Dirección Nacional del Antártico. Instituto Antártico Argentino; Argentina
Fil: Villalobos, Jaime. Universidad Nacional de Colombia; Colombia
description We applied multi–temporal 1D magnetotelluric (MT) surveys to identify space–time anomalies of apparent resistivity ((Formula presented.)) in the upper lithosphere in the Antarctic Peninsula (the border between the Antarctic and the Shetland plates). We used time series over several weeks of the natural Earth’s electric and magnetic fields registered at one MT station of the Universidad Nacional de Colombia (RSUNAL) located at Seymour–Marambio Island, Antarctica. We associated resistivity anomalies with contrasting earthquake activity. Anomalies of (Formula presented.) were detected almost simultaneously with the beginning of a seismic crisis in the Bransfield Strait, south of King George Island (approximately 85.000 events were reported close to the Orca submarine volcano, with focal depths < 20 km and MWW < 6.9). We explained the origin of these anomalies in response to fluid migration near the place of the fractures linked with the seismic swarm, which could promote disturbances of the pore pressure field that reached some hundreds of km away.
publishDate 2023
dc.date.none.fl_str_mv 2023-02
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
http://purl.org/coar/resource_type/c_6501
info:ar-repo/semantics/articulo
format article
status_str publishedVersion
dc.identifier.none.fl_str_mv http://hdl.handle.net/11336/219722
Vargas, Carlos A.; Caneva, Alexander; Solano, Juan M.; Gulisano, Adriana Maria; Villalobos, Jaime; Evidencing Fluid Migration of the Crust during the Seismic Swarm by Using 1D Magnetotelluric Monitoring; MDPI; Applied Sciences; 13; 4; 2-2023; 1-12
2076-3417
CONICET Digital
CONICET
url http://hdl.handle.net/11336/219722
identifier_str_mv Vargas, Carlos A.; Caneva, Alexander; Solano, Juan M.; Gulisano, Adriana Maria; Villalobos, Jaime; Evidencing Fluid Migration of the Crust during the Seismic Swarm by Using 1D Magnetotelluric Monitoring; MDPI; Applied Sciences; 13; 4; 2-2023; 1-12
2076-3417
CONICET Digital
CONICET
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/url/https://doi.org/10.3390/app13042683
info:eu-repo/semantics/altIdentifier/doi/10.3390/app13042683
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
eu_rights_str_mv openAccess
rights_invalid_str_mv https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
dc.format.none.fl_str_mv application/pdf
application/pdf
dc.publisher.none.fl_str_mv MDPI
publisher.none.fl_str_mv MDPI
dc.source.none.fl_str_mv reponame:CONICET Digital (CONICET)
instname:Consejo Nacional de Investigaciones Científicas y Técnicas
reponame_str CONICET Digital (CONICET)
collection CONICET Digital (CONICET)
instname_str Consejo Nacional de Investigaciones Científicas y Técnicas
repository.name.fl_str_mv CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas
repository.mail.fl_str_mv dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar
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score 13.070432

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