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
.jpg)
- Institución
- Consejo Nacional de Investigaciones Científicas y Técnicas
- OAI Identificador
- oai:ri.conicet.gov.ar:11336/46363
Ver los metadatos del registro completo
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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 |
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2015-10 |
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info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion http://purl.org/coar/resource_type/c_6501 info:ar-repo/semantics/articulo |
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article |
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publishedVersion |
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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 |
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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 |
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info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ |
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openAccess |
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https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ |
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application/pdf application/pdf |
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Pergamon-Elsevier Science Ltd |
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Pergamon-Elsevier Science Ltd |
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reponame:CONICET Digital (CONICET) instname:Consejo Nacional de Investigaciones Científicas y Técnicas |
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CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas |
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dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar |
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