Geological evidence for fluid overpressure, hydraulic fracturing and strong heating during maturation and migration of hydrocarbons in Mesozoic rocks of the northern Neuquén Basin,...

Autores
Zanella, Alain; Cobbold, Peter R.; Ruffet, Gilles; Leanza, Hector Armando
Año de publicación
2015
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
In the northern Neuquen Basin of Argentina (especially in Mendoza Province), there is strong geological evidence for fluid overpressure in the past. The evidence takes the form of bitumen veins and beddingparallel veins of fibrous calcite (‘beef’). Such veins are widespread in the fold-and-thrust belt of the Malargue area, where bitumen mining has been active for a century or so. So as to collect information on the development of fluid overpressure in this part of the Neuquen Basin, several old mines were visited and studied in the Malargue area. Here the bitumen veins have intruded mainly the Late Jurassic to Early Cretaceous Mendoza Group, but also the Late Cretaceous Neuquen Group. The veins have the forms of bedding-parallel sills or dykes and they are especially thick within anticlines, forming saddle-reefs in several places. Beef veins are also numerous in the Malargue area. They contain bitumen and therefore seem to have formed at the same time as the bitumen veins. Near many outcrops of bitumen and beef, we have found fine-grained volcanic intrusive bodies. The best examples are from the La Valenciana syncline. According to 39Ar-40Ar dating, these bodies are mainly of Mid-Miocene age. More generally, volcanism, deformation and maturation of source rocks seem to have reached a climax in Miocene times, when the subducting Pacific slab became relatively flat.
Fil: Zanella, Alain. Universite de Rennes I; Francia. Université du Maine; Francia. Centre National de la Recherche Scientifique; Francia
Fil: Cobbold, Peter R.. Universite de Rennes I; Francia
Fil: Ruffet, Gilles. Universite de Rennes I; Francia
Fil: Leanza, Hector Armando. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Parque Centenario. Museo Argentino de Ciencias Naturales "Bernardino Rivadavia"; Argentina
Materia
Geology
Oil Systems
Fluid Overpressure
Neuquen Basin
Argentina
Mendoza Province
Beef
Bitumen Veins
39ar-40ar
Hydrocarbon Migration
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:11336/46363

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network_name_str CONICET Digital (CONICET)
spelling Geological evidence for fluid overpressure, hydraulic fracturing and strong heating during maturation and migration of hydrocarbons in Mesozoic rocks of the northern Neuquén Basin, Mendoza Province, ArgentinaZanella, AlainCobbold, Peter R.Ruffet, GillesLeanza, Hector ArmandoGeologyOil SystemsFluid OverpressureNeuquen BasinArgentinaMendoza ProvinceBeefBitumen Veins39ar-40arHydrocarbon Migrationhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1In the northern Neuquen Basin of Argentina (especially in Mendoza Province), there is strong geological evidence for fluid overpressure in the past. The evidence takes the form of bitumen veins and beddingparallel veins of fibrous calcite (‘beef’). Such veins are widespread in the fold-and-thrust belt of the Malargue area, where bitumen mining has been active for a century or so. So as to collect information on the development of fluid overpressure in this part of the Neuquen Basin, several old mines were visited and studied in the Malargue area. Here the bitumen veins have intruded mainly the Late Jurassic to Early Cretaceous Mendoza Group, but also the Late Cretaceous Neuquen Group. The veins have the forms of bedding-parallel sills or dykes and they are especially thick within anticlines, forming saddle-reefs in several places. Beef veins are also numerous in the Malargue area. They contain bitumen and therefore seem to have formed at the same time as the bitumen veins. Near many outcrops of bitumen and beef, we have found fine-grained volcanic intrusive bodies. The best examples are from the La Valenciana syncline. According to 39Ar-40Ar dating, these bodies are mainly of Mid-Miocene age. More generally, volcanism, deformation and maturation of source rocks seem to have reached a climax in Miocene times, when the subducting Pacific slab became relatively flat.Fil: Zanella, Alain. Universite de Rennes I; Francia. Université du Maine; Francia. Centre National de la Recherche Scientifique; FranciaFil: Cobbold, Peter R.. Universite de Rennes I; FranciaFil: Ruffet, Gilles. Universite de Rennes I; FranciaFil: Leanza, Hector Armando. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Parque Centenario. Museo Argentino de Ciencias Naturales "Bernardino Rivadavia"; ArgentinaPergamon-Elsevier Science Ltd2015-10info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/46363Zanella, Alain; Cobbold, Peter R.; Ruffet, Gilles; Leanza, Hector Armando; Geological evidence for fluid overpressure, hydraulic fracturing and strong heating during maturation and migration of hydrocarbons in Mesozoic rocks of the northern Neuquén Basin, Mendoza Province, Argentina; Pergamon-Elsevier Science Ltd; Journal of South American Earth Sciences; 62; 10-2015; 229-2420895-98111873-0647CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/doi/10.1016/j.jsames.2015.06.006info:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/pii/S0895981115300122info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2026-04-23T14:39:36Zoai:ri.conicet.gov.ar:11336/46363instacron: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:34982026-04-23 14:39:37.28CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Geological evidence for fluid overpressure, hydraulic fracturing and strong heating during maturation and migration of hydrocarbons in Mesozoic rocks of the northern Neuquén Basin, Mendoza Province, Argentina
title Geological evidence for fluid overpressure, hydraulic fracturing and strong heating during maturation and migration of hydrocarbons in Mesozoic rocks of the northern Neuquén Basin, Mendoza Province, Argentina
spellingShingle Geological evidence for fluid overpressure, hydraulic fracturing and strong heating during maturation and migration of hydrocarbons in Mesozoic rocks of the northern Neuquén Basin, Mendoza Province, Argentina
Zanella, Alain
Geology
Oil Systems
Fluid Overpressure
Neuquen Basin
Argentina
Mendoza Province
Beef
Bitumen Veins
39ar-40ar
Hydrocarbon Migration
title_short Geological evidence for fluid overpressure, hydraulic fracturing and strong heating during maturation and migration of hydrocarbons in Mesozoic rocks of the northern Neuquén Basin, Mendoza Province, Argentina
title_full Geological evidence for fluid overpressure, hydraulic fracturing and strong heating during maturation and migration of hydrocarbons in Mesozoic rocks of the northern Neuquén Basin, Mendoza Province, Argentina
title_fullStr Geological evidence for fluid overpressure, hydraulic fracturing and strong heating during maturation and migration of hydrocarbons in Mesozoic rocks of the northern Neuquén Basin, Mendoza Province, Argentina
title_full_unstemmed Geological evidence for fluid overpressure, hydraulic fracturing and strong heating during maturation and migration of hydrocarbons in Mesozoic rocks of the northern Neuquén Basin, Mendoza Province, Argentina
title_sort Geological evidence for fluid overpressure, hydraulic fracturing and strong heating during maturation and migration of hydrocarbons in Mesozoic rocks of the northern Neuquén Basin, Mendoza Province, Argentina
dc.creator.none.fl_str_mv Zanella, Alain
Cobbold, Peter R.
Ruffet, Gilles
Leanza, Hector Armando
author Zanella, Alain
author_facet Zanella, Alain
Cobbold, Peter R.
Ruffet, Gilles
Leanza, Hector Armando
author_role author
author2 Cobbold, Peter R.
Ruffet, Gilles
Leanza, Hector Armando
author2_role author
author
author
dc.subject.none.fl_str_mv Geology
Oil Systems
Fluid Overpressure
Neuquen Basin
Argentina
Mendoza Province
Beef
Bitumen Veins
39ar-40ar
Hydrocarbon Migration
topic Geology
Oil Systems
Fluid Overpressure
Neuquen Basin
Argentina
Mendoza Province
Beef
Bitumen Veins
39ar-40ar
Hydrocarbon Migration
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv In the northern Neuquen Basin of Argentina (especially in Mendoza Province), there is strong geological evidence for fluid overpressure in the past. The evidence takes the form of bitumen veins and beddingparallel veins of fibrous calcite (‘beef’). Such veins are widespread in the fold-and-thrust belt of the Malargue area, where bitumen mining has been active for a century or so. So as to collect information on the development of fluid overpressure in this part of the Neuquen Basin, several old mines were visited and studied in the Malargue area. Here the bitumen veins have intruded mainly the Late Jurassic to Early Cretaceous Mendoza Group, but also the Late Cretaceous Neuquen Group. The veins have the forms of bedding-parallel sills or dykes and they are especially thick within anticlines, forming saddle-reefs in several places. Beef veins are also numerous in the Malargue area. They contain bitumen and therefore seem to have formed at the same time as the bitumen veins. Near many outcrops of bitumen and beef, we have found fine-grained volcanic intrusive bodies. The best examples are from the La Valenciana syncline. According to 39Ar-40Ar dating, these bodies are mainly of Mid-Miocene age. More generally, volcanism, deformation and maturation of source rocks seem to have reached a climax in Miocene times, when the subducting Pacific slab became relatively flat.
Fil: Zanella, Alain. Universite de Rennes I; Francia. Université du Maine; Francia. Centre National de la Recherche Scientifique; Francia
Fil: Cobbold, Peter R.. Universite de Rennes I; Francia
Fil: Ruffet, Gilles. Universite de Rennes I; Francia
Fil: Leanza, Hector Armando. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Parque Centenario. Museo Argentino de Ciencias Naturales "Bernardino Rivadavia"; Argentina
description In the northern Neuquen Basin of Argentina (especially in Mendoza Province), there is strong geological evidence for fluid overpressure in the past. The evidence takes the form of bitumen veins and beddingparallel veins of fibrous calcite (‘beef’). Such veins are widespread in the fold-and-thrust belt of the Malargue area, where bitumen mining has been active for a century or so. So as to collect information on the development of fluid overpressure in this part of the Neuquen Basin, several old mines were visited and studied in the Malargue area. Here the bitumen veins have intruded mainly the Late Jurassic to Early Cretaceous Mendoza Group, but also the Late Cretaceous Neuquen Group. The veins have the forms of bedding-parallel sills or dykes and they are especially thick within anticlines, forming saddle-reefs in several places. Beef veins are also numerous in the Malargue area. They contain bitumen and therefore seem to have formed at the same time as the bitumen veins. Near many outcrops of bitumen and beef, we have found fine-grained volcanic intrusive bodies. The best examples are from the La Valenciana syncline. According to 39Ar-40Ar dating, these bodies are mainly of Mid-Miocene age. More generally, volcanism, deformation and maturation of source rocks seem to have reached a climax in Miocene times, when the subducting Pacific slab became relatively flat.
publishDate 2015
dc.date.none.fl_str_mv 2015-10
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/11336/46363
Zanella, Alain; Cobbold, Peter R.; Ruffet, Gilles; Leanza, Hector Armando; Geological evidence for fluid overpressure, hydraulic fracturing and strong heating during maturation and migration of hydrocarbons in Mesozoic rocks of the northern Neuquén Basin, Mendoza Province, Argentina; Pergamon-Elsevier Science Ltd; Journal of South American Earth Sciences; 62; 10-2015; 229-242
0895-9811
1873-0647
CONICET Digital
CONICET
url http://hdl.handle.net/11336/46363
identifier_str_mv Zanella, Alain; Cobbold, Peter R.; Ruffet, Gilles; Leanza, Hector Armando; Geological evidence for fluid overpressure, hydraulic fracturing and strong heating during maturation and migration of hydrocarbons in Mesozoic rocks of the northern Neuquén Basin, Mendoza Province, Argentina; Pergamon-Elsevier Science Ltd; Journal of South American Earth Sciences; 62; 10-2015; 229-242
0895-9811
1873-0647
CONICET Digital
CONICET
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/doi/10.1016/j.jsames.2015.06.006
info:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/pii/S0895981115300122
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 Pergamon-Elsevier Science Ltd
publisher.none.fl_str_mv Pergamon-Elsevier Science Ltd
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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