Seismo-electrics, electro-seismics, and seismo-magnetics for earth sciences

Autores
Jouniaux, Laurence; Zyserman, Fabio Iván
Año de publicación
2015
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
The seismo-electromagnetic method (SEM) is used for non-invasive subsurface exploration. It shows interesting results for detecting fluids such as water, ice, oil, gas, CO2, and also to better characterise the subsurface in terms of porosity, permeability, and fractures. However, a limitation of this method is the low level of the induced signals. We first describe SEM's theoretical background, and the role of some key parameters. We then detail recent studies on SEM, through theoretical and numerical developments, and through field and laboratory observations, to show that this method can bring advantages compared to classical geophysical methods.
Este artículo de discusión ha sido evaluado y publicado en Solid Earth 7(1). Se puede acceder al mismo desde el enlace "Documento relacionado".
Facultad de Ciencias Astronómicas y Geofísicas
Materia
Ciencias Naturales
Geofísica
seismo-electromagnetic method
subsurface exploration
Nivel de accesibilidad
acceso abierto
Condiciones de uso
http://creativecommons.org/licenses/by/4.0/
Repositorio
SEDICI (UNLP)
Institución
Universidad Nacional de La Plata
OAI Identificador
oai:sedici.unlp.edu.ar:10915/131469
Acceder
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oai_identifier_str oai:sedici.unlp.edu.ar:10915/131469
network_acronym_str SEDICI
repository_id_str 1329
network_name_str SEDICI (UNLP)
spelling Seismo-electrics, electro-seismics, and seismo-magnetics for earth sciencesJouniaux, LaurenceZyserman, Fabio IvánCiencias NaturalesGeofísicaseismo-electromagnetic methodsubsurface explorationThe seismo-electromagnetic method (SEM) is used for non-invasive subsurface exploration. It shows interesting results for detecting fluids such as water, ice, oil, gas, CO2, and also to better characterise the subsurface in terms of porosity, permeability, and fractures. However, a limitation of this method is the low level of the induced signals. We first describe SEM's theoretical background, and the role of some key parameters. We then detail recent studies on SEM, through theoretical and numerical developments, and through field and laboratory observations, to show that this method can bring advantages compared to classical geophysical methods.Este artículo de discusión ha sido evaluado y publicado en Solid Earth 7(1). Se puede acceder al mismo desde el enlace "Documento relacionado".Facultad de Ciencias Astronómicas y Geofísicas2015-09-18info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionArticulohttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdf2563-2662http://sedici.unlp.edu.ar/handle/10915/131469enginfo:eu-repo/semantics/altIdentifier/doi/10.5194/sed-7-2563-2015info:eu-repo/semantics/reference/hdl/10915/131471info:eu-repo/semantics/openAccesshttp://creativecommons.org/licenses/by/4.0/Creative Commons Attribution 4.0 International (CC BY 4.0)reponame:SEDICI (UNLP)instname:Universidad Nacional de La Platainstacron:UNLP2025-09-29T11:32:37Zoai:sedici.unlp.edu.ar:10915/131469Institucionalhttp://sedici.unlp.edu.ar/Universidad públicaNo correspondehttp://sedici.unlp.edu.ar/oai/snrdalira@sedici.unlp.edu.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:13292025-09-29 11:32:38.083SEDICI (UNLP) - Universidad Nacional de La Platafalse
dc.title.none.fl_str_mv Seismo-electrics, electro-seismics, and seismo-magnetics for earth sciences
title Seismo-electrics, electro-seismics, and seismo-magnetics for earth sciences
spellingShingle Seismo-electrics, electro-seismics, and seismo-magnetics for earth sciences
Jouniaux, Laurence
Ciencias Naturales
Geofísica
seismo-electromagnetic method
subsurface exploration
title_short Seismo-electrics, electro-seismics, and seismo-magnetics for earth sciences
title_full Seismo-electrics, electro-seismics, and seismo-magnetics for earth sciences
title_fullStr Seismo-electrics, electro-seismics, and seismo-magnetics for earth sciences
title_full_unstemmed Seismo-electrics, electro-seismics, and seismo-magnetics for earth sciences
title_sort Seismo-electrics, electro-seismics, and seismo-magnetics for earth sciences
dc.creator.none.fl_str_mv Jouniaux, Laurence
Zyserman, Fabio Iván
author Jouniaux, Laurence
author_facet Jouniaux, Laurence
Zyserman, Fabio Iván
author_role author
author2 Zyserman, Fabio Iván
author2_role author
dc.subject.none.fl_str_mv Ciencias Naturales
Geofísica
seismo-electromagnetic method
subsurface exploration
topic Ciencias Naturales
Geofísica
seismo-electromagnetic method
subsurface exploration
dc.description.none.fl_txt_mv The seismo-electromagnetic method (SEM) is used for non-invasive subsurface exploration. It shows interesting results for detecting fluids such as water, ice, oil, gas, CO2, and also to better characterise the subsurface in terms of porosity, permeability, and fractures. However, a limitation of this method is the low level of the induced signals. We first describe SEM's theoretical background, and the role of some key parameters. We then detail recent studies on SEM, through theoretical and numerical developments, and through field and laboratory observations, to show that this method can bring advantages compared to classical geophysical methods.
Este artículo de discusión ha sido evaluado y publicado en Solid Earth 7(1). Se puede acceder al mismo desde el enlace "Documento relacionado".
Facultad de Ciencias Astronómicas y Geofísicas
description The seismo-electromagnetic method (SEM) is used for non-invasive subsurface exploration. It shows interesting results for detecting fluids such as water, ice, oil, gas, CO2, and also to better characterise the subsurface in terms of porosity, permeability, and fractures. However, a limitation of this method is the low level of the induced signals. We first describe SEM's theoretical background, and the role of some key parameters. We then detail recent studies on SEM, through theoretical and numerical developments, and through field and laboratory observations, to show that this method can bring advantages compared to classical geophysical methods.
publishDate 2015
dc.date.none.fl_str_mv 2015-09-18
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
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info:ar-repo/semantics/articulo
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dc.identifier.none.fl_str_mv http://sedici.unlp.edu.ar/handle/10915/131469
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dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/doi/10.5194/sed-7-2563-2015
info:eu-repo/semantics/reference/hdl/10915/131471
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
http://creativecommons.org/licenses/by/4.0/
Creative Commons Attribution 4.0 International (CC BY 4.0)
eu_rights_str_mv openAccess
rights_invalid_str_mv http://creativecommons.org/licenses/by/4.0/
Creative Commons Attribution 4.0 International (CC BY 4.0)
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instname:Universidad Nacional de La Plata
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collection SEDICI (UNLP)
instname_str Universidad Nacional de La Plata
instacron_str UNLP
institution UNLP
repository.name.fl_str_mv SEDICI (UNLP) - Universidad Nacional de La Plata
repository.mail.fl_str_mv alira@sedici.unlp.edu.ar
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