The long-term legacy of subvolcanic intrusions on fluid migration in sedimentary basins: The Cerro Alquitrán case study, northern Neuquén Basin, Argentina

Autores
Galland, Olivier; Villar, Héctor J.; Mescua, Jose Francisco; Jerram, Dougal A.; Midtkandal, Ivar; Palma, J. Octavio; Planke, Sverre; Zanella, Alain
Año de publicación
2023
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
Cooling subvolcanic igneous intrusions are known to have a substantial impact on fluid flow in the shallow Earth´s crust, for example activation of geothermal systems, circulation of mineralized fluids in ore deposits, fast maturation of organic matter in sedimentary rocks and the potential release of large volumes of greenhouse gases, which have triggered mass extinctions during the Earth´s history. However, the long-term post-cooling legacy of subvolcanic intrusions on fluid flow received much less attention. Here we describe a demonstrative geological example in the Andean foothills, Argentina, showing that igneous intrusions have long-term effects on fluid flow after their emplacement and cooling. The case study is a ca. 11-million-year-old, eroded subvolcanic conduit, at the rims of which large volumes of bitumen are naturally seeping out on the Earth´s surface. This contribution highlights that intense syn-emplacement fracturing of the magma has created high-permeability pathways that affect the regional fluid circulations, even millions of years after cooling. Our observations reveal how extinct subvolcanic intrusions have long-term consequences on subsurface fluid circulations, which need to be accounted for in the exploration of geothermal energy, drinkable groundwater, hydrocarbons and CO2 sequestration in volcanic basins and regions hosting ancient shallow magma intrusions.
Fil: Galland, Olivier. University Of Oslo. Faculty Of Mathematics And Natural Science. Departamento Geosciences; Noruega
Fil: Villar, Héctor J.. Geolab Sur S.a.; Argentina
Fil: Mescua, Jose Francisco. Universidad Nacional de Cuyo. Facultad de Ciencias Exactas y Naturales; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Provincia de Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Universidad Nacional de Cuyo. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales; Argentina
Fil: Jerram, Dougal A.. University Of Oslo. Faculty Of Mathematics And Natural Science. Departamento Geosciences; Noruega
Fil: Midtkandal, Ivar. University Of Oslo. Faculty Of Mathematics And Natural Science. Departamento Geosciences; Noruega
Fil: Palma, J. Octavio. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo; Argentina
Fil: Planke, Sverre. University Of Oslo. Faculty Of Mathematics And Natural Science. Departamento Geosciences; Noruega
Fil: Zanella, Alain. Le Mans Université.; Francia
Materia
Intrusion
Fluid flow
Deformation
Nivel de accesibilidad
acceso abierto
Condiciones de uso
https://creativecommons.org/licenses/by-nc-nd/2.5/ar/
Repositorio
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/230719
Acceder
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network_name_str CONICET Digital (CONICET)
spelling The long-term legacy of subvolcanic intrusions on fluid migration in sedimentary basins: The Cerro Alquitrán case study, northern Neuquén Basin, ArgentinaGalland, OlivierVillar, Héctor J.Mescua, Jose FranciscoJerram, Dougal A.Midtkandal, IvarPalma, J. OctavioPlanke, SverreZanella, AlainIntrusionFluid flowDeformationhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1Cooling subvolcanic igneous intrusions are known to have a substantial impact on fluid flow in the shallow Earth´s crust, for example activation of geothermal systems, circulation of mineralized fluids in ore deposits, fast maturation of organic matter in sedimentary rocks and the potential release of large volumes of greenhouse gases, which have triggered mass extinctions during the Earth´s history. However, the long-term post-cooling legacy of subvolcanic intrusions on fluid flow received much less attention. Here we describe a demonstrative geological example in the Andean foothills, Argentina, showing that igneous intrusions have long-term effects on fluid flow after their emplacement and cooling. The case study is a ca. 11-million-year-old, eroded subvolcanic conduit, at the rims of which large volumes of bitumen are naturally seeping out on the Earth´s surface. This contribution highlights that intense syn-emplacement fracturing of the magma has created high-permeability pathways that affect the regional fluid circulations, even millions of years after cooling. Our observations reveal how extinct subvolcanic intrusions have long-term consequences on subsurface fluid circulations, which need to be accounted for in the exploration of geothermal energy, drinkable groundwater, hydrocarbons and CO2 sequestration in volcanic basins and regions hosting ancient shallow magma intrusions.Fil: Galland, Olivier. University Of Oslo. Faculty Of Mathematics And Natural Science. Departamento Geosciences; NoruegaFil: Villar, Héctor J.. Geolab Sur S.a.; ArgentinaFil: Mescua, Jose Francisco. Universidad Nacional de Cuyo. Facultad de Ciencias Exactas y Naturales; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Provincia de Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Universidad Nacional de Cuyo. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales; ArgentinaFil: Jerram, Dougal A.. University Of Oslo. Faculty Of Mathematics And Natural Science. Departamento Geosciences; NoruegaFil: Midtkandal, Ivar. University Of Oslo. Faculty Of Mathematics And Natural Science. Departamento Geosciences; NoruegaFil: Palma, J. Octavio. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo; ArgentinaFil: Planke, Sverre. University Of Oslo. Faculty Of Mathematics And Natural Science. Departamento Geosciences; NoruegaFil: Zanella, Alain. Le Mans Université.; FranciaWiley Blackwell Publishing, Inc2023-05info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/230719Galland, Olivier; Villar, Héctor J.; Mescua, Jose Francisco; Jerram, Dougal A.; Midtkandal, Ivar; et al.; The long-term legacy of subvolcanic intrusions on fluid migration in sedimentary basins: The Cerro Alquitrán case study, northern Neuquén Basin, Argentina; Wiley Blackwell Publishing, Inc; Basin Research; 35; 5; 5-2023; 1840-18550950-091X1365-2117CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/https://onlinelibrary.wiley.com/doi/10.1111/bre.12782info:eu-repo/semantics/altIdentifier/doi/10.1111/bre.12782info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-nd/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-10-15T14:55:39Zoai:ri.conicet.gov.ar:11336/230719instacron: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:34982025-10-15 14:55:39.717CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv The long-term legacy of subvolcanic intrusions on fluid migration in sedimentary basins: The Cerro Alquitrán case study, northern Neuquén Basin, Argentina
title The long-term legacy of subvolcanic intrusions on fluid migration in sedimentary basins: The Cerro Alquitrán case study, northern Neuquén Basin, Argentina
spellingShingle The long-term legacy of subvolcanic intrusions on fluid migration in sedimentary basins: The Cerro Alquitrán case study, northern Neuquén Basin, Argentina
Galland, Olivier
Intrusion
Fluid flow
Deformation
title_short The long-term legacy of subvolcanic intrusions on fluid migration in sedimentary basins: The Cerro Alquitrán case study, northern Neuquén Basin, Argentina
title_full The long-term legacy of subvolcanic intrusions on fluid migration in sedimentary basins: The Cerro Alquitrán case study, northern Neuquén Basin, Argentina
title_fullStr The long-term legacy of subvolcanic intrusions on fluid migration in sedimentary basins: The Cerro Alquitrán case study, northern Neuquén Basin, Argentina
title_full_unstemmed The long-term legacy of subvolcanic intrusions on fluid migration in sedimentary basins: The Cerro Alquitrán case study, northern Neuquén Basin, Argentina
title_sort The long-term legacy of subvolcanic intrusions on fluid migration in sedimentary basins: The Cerro Alquitrán case study, northern Neuquén Basin, Argentina
dc.creator.none.fl_str_mv Galland, Olivier
Villar, Héctor J.
Mescua, Jose Francisco
Jerram, Dougal A.
Midtkandal, Ivar
Palma, J. Octavio
Planke, Sverre
Zanella, Alain
author Galland, Olivier
author_facet Galland, Olivier
Villar, Héctor J.
Mescua, Jose Francisco
Jerram, Dougal A.
Midtkandal, Ivar
Palma, J. Octavio
Planke, Sverre
Zanella, Alain
author_role author
author2 Villar, Héctor J.
Mescua, Jose Francisco
Jerram, Dougal A.
Midtkandal, Ivar
Palma, J. Octavio
Planke, Sverre
Zanella, Alain
author2_role author
author
author
author
author
author
author
dc.subject.none.fl_str_mv Intrusion
Fluid flow
Deformation
topic Intrusion
Fluid flow
Deformation
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv Cooling subvolcanic igneous intrusions are known to have a substantial impact on fluid flow in the shallow Earth´s crust, for example activation of geothermal systems, circulation of mineralized fluids in ore deposits, fast maturation of organic matter in sedimentary rocks and the potential release of large volumes of greenhouse gases, which have triggered mass extinctions during the Earth´s history. However, the long-term post-cooling legacy of subvolcanic intrusions on fluid flow received much less attention. Here we describe a demonstrative geological example in the Andean foothills, Argentina, showing that igneous intrusions have long-term effects on fluid flow after their emplacement and cooling. The case study is a ca. 11-million-year-old, eroded subvolcanic conduit, at the rims of which large volumes of bitumen are naturally seeping out on the Earth´s surface. This contribution highlights that intense syn-emplacement fracturing of the magma has created high-permeability pathways that affect the regional fluid circulations, even millions of years after cooling. Our observations reveal how extinct subvolcanic intrusions have long-term consequences on subsurface fluid circulations, which need to be accounted for in the exploration of geothermal energy, drinkable groundwater, hydrocarbons and CO2 sequestration in volcanic basins and regions hosting ancient shallow magma intrusions.
Fil: Galland, Olivier. University Of Oslo. Faculty Of Mathematics And Natural Science. Departamento Geosciences; Noruega
Fil: Villar, Héctor J.. Geolab Sur S.a.; Argentina
Fil: Mescua, Jose Francisco. Universidad Nacional de Cuyo. Facultad de Ciencias Exactas y Naturales; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Provincia de Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Universidad Nacional de Cuyo. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales; Argentina
Fil: Jerram, Dougal A.. University Of Oslo. Faculty Of Mathematics And Natural Science. Departamento Geosciences; Noruega
Fil: Midtkandal, Ivar. University Of Oslo. Faculty Of Mathematics And Natural Science. Departamento Geosciences; Noruega
Fil: Palma, J. Octavio. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo; Argentina
Fil: Planke, Sverre. University Of Oslo. Faculty Of Mathematics And Natural Science. Departamento Geosciences; Noruega
Fil: Zanella, Alain. Le Mans Université.; Francia
description Cooling subvolcanic igneous intrusions are known to have a substantial impact on fluid flow in the shallow Earth´s crust, for example activation of geothermal systems, circulation of mineralized fluids in ore deposits, fast maturation of organic matter in sedimentary rocks and the potential release of large volumes of greenhouse gases, which have triggered mass extinctions during the Earth´s history. However, the long-term post-cooling legacy of subvolcanic intrusions on fluid flow received much less attention. Here we describe a demonstrative geological example in the Andean foothills, Argentina, showing that igneous intrusions have long-term effects on fluid flow after their emplacement and cooling. The case study is a ca. 11-million-year-old, eroded subvolcanic conduit, at the rims of which large volumes of bitumen are naturally seeping out on the Earth´s surface. This contribution highlights that intense syn-emplacement fracturing of the magma has created high-permeability pathways that affect the regional fluid circulations, even millions of years after cooling. Our observations reveal how extinct subvolcanic intrusions have long-term consequences on subsurface fluid circulations, which need to be accounted for in the exploration of geothermal energy, drinkable groundwater, hydrocarbons and CO2 sequestration in volcanic basins and regions hosting ancient shallow magma intrusions.
publishDate 2023
dc.date.none.fl_str_mv 2023-05
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/11336/230719
Galland, Olivier; Villar, Héctor J.; Mescua, Jose Francisco; Jerram, Dougal A.; Midtkandal, Ivar; et al.; The long-term legacy of subvolcanic intrusions on fluid migration in sedimentary basins: The Cerro Alquitrán case study, northern Neuquén Basin, Argentina; Wiley Blackwell Publishing, Inc; Basin Research; 35; 5; 5-2023; 1840-1855
0950-091X
1365-2117
CONICET Digital
CONICET
url http://hdl.handle.net/11336/230719
identifier_str_mv Galland, Olivier; Villar, Héctor J.; Mescua, Jose Francisco; Jerram, Dougal A.; Midtkandal, Ivar; et al.; The long-term legacy of subvolcanic intrusions on fluid migration in sedimentary basins: The Cerro Alquitrán case study, northern Neuquén Basin, Argentina; Wiley Blackwell Publishing, Inc; Basin Research; 35; 5; 5-2023; 1840-1855
0950-091X
1365-2117
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://onlinelibrary.wiley.com/doi/10.1111/bre.12782
info:eu-repo/semantics/altIdentifier/doi/10.1111/bre.12782
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by-nc-nd/2.5/ar/
eu_rights_str_mv openAccess
rights_invalid_str_mv https://creativecommons.org/licenses/by-nc-nd/2.5/ar/
dc.format.none.fl_str_mv application/pdf
application/pdf
dc.publisher.none.fl_str_mv Wiley Blackwell Publishing, Inc
publisher.none.fl_str_mv Wiley Blackwell Publishing, Inc
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
_version_ 1846083090818007040
score 13.22299

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