Relationships between depositional processes, geochemical signature and seismic geometries in the Vaca Muerta Formation, Neuquén Basin, Argentina

Autores
Sagasti, Guillermina; Remirez, Mariano Nicolas; Spalletti, Luis Antonio
Año de publicación
2015
Idioma
inglés
Tipo de recurso
documento de conferencia
Estado
versión publicada
Descripción
The Upper Jurassic-Lower Cretaceous Vaca Muerta Formation (VMF) in the NeuquénBasin (Argentina) has recently emerged as the main shale oil/gas producer outside USA. The VMF is an extensive world-class hydrocarbon source rock with a prospective area in the order of 30.000 km2. The unit is part of a mixed clastic-carbonate succession deposited in a distally-steepened ramp, characterized by the development of northwest prograding clinoforms. In order to investigate possible relationships between depositional processes, geochemical signature, and geometries, which ultimately impact reservoir production, an integrated study involving inorganic geochemistry, core characterization, and seismic interpretation was conducted along a dip-oriented transect (ca. 25 km) in the center of the Neuquén Basin. The basinal facies are primarily composed of laminated mudstones with the highest content of redoxsensitive elements (V, Mo, Cr, Co, Ni, Zn) depicting sub-horizontal parallel reflections. Toe-of-slope facies comprises mainly laminated and bioturbated mudstones showing a decrease in the amount of redoxsensitive elements coupled with an increment in elements indicative of siliciclastic sedimentation (Si, Al,K, Zr, Ti) and availability of nutrients (Ba, P). Finally, upper slope and roll-over facies involve bioturbatedmudstones and mudstones with benthonic foraminifera and are characterized by a relative decrease in elements indicative of siliciclastic sedimentation along with an increase in elements with carbonate affinity (Ca, Sc, P). These results suggest a genetic relationship between inorganic geochemical signature and depositional processes along the clinoform, thus providing and additional proxy to evaluate shale reservoirs particularly in the absence of core and/or 3D seismic data.
Fil: Sagasti, Guillermina. Ypf Sociedad Anonima. Gerencia de Geociencias y Reservorios; Argentina
Fil: Remirez, Mariano Nicolas. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata. Centro de Investigaciones Geológicas. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Centro de Investigaciones Geológicas; Argentina
Fil: Spalletti, Luis Antonio. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata. Centro de Investigaciones Geológicas. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Centro de Investigaciones Geológicas; Argentina
2015 Annual Convention and Exhibition
Denver
Estados Unidos
American Association of Petroleum Geologists
Materia
Neuquén Basin
Geochemistry
Vaca Muerta Formation
Argentina
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:11336/234413
Acceder
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oai_identifier_str oai:ri.conicet.gov.ar:11336/234413
network_acronym_str CONICETDig
repository_id_str 3498
network_name_str CONICET Digital (CONICET)
spelling Relationships between depositional processes, geochemical signature and seismic geometries in the Vaca Muerta Formation, Neuquén Basin, ArgentinaSagasti, GuillerminaRemirez, Mariano NicolasSpalletti, Luis AntonioNeuquén BasinGeochemistryVaca Muerta FormationArgentinahttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1The Upper Jurassic-Lower Cretaceous Vaca Muerta Formation (VMF) in the NeuquénBasin (Argentina) has recently emerged as the main shale oil/gas producer outside USA. The VMF is an extensive world-class hydrocarbon source rock with a prospective area in the order of 30.000 km2. The unit is part of a mixed clastic-carbonate succession deposited in a distally-steepened ramp, characterized by the development of northwest prograding clinoforms. In order to investigate possible relationships between depositional processes, geochemical signature, and geometries, which ultimately impact reservoir production, an integrated study involving inorganic geochemistry, core characterization, and seismic interpretation was conducted along a dip-oriented transect (ca. 25 km) in the center of the Neuquén Basin. The basinal facies are primarily composed of laminated mudstones with the highest content of redoxsensitive elements (V, Mo, Cr, Co, Ni, Zn) depicting sub-horizontal parallel reflections. Toe-of-slope facies comprises mainly laminated and bioturbated mudstones showing a decrease in the amount of redoxsensitive elements coupled with an increment in elements indicative of siliciclastic sedimentation (Si, Al,K, Zr, Ti) and availability of nutrients (Ba, P). Finally, upper slope and roll-over facies involve bioturbatedmudstones and mudstones with benthonic foraminifera and are characterized by a relative decrease in elements indicative of siliciclastic sedimentation along with an increase in elements with carbonate affinity (Ca, Sc, P). These results suggest a genetic relationship between inorganic geochemical signature and depositional processes along the clinoform, thus providing and additional proxy to evaluate shale reservoirs particularly in the absence of core and/or 3D seismic data.Fil: Sagasti, Guillermina. Ypf Sociedad Anonima. Gerencia de Geociencias y Reservorios; ArgentinaFil: Remirez, Mariano Nicolas. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata. Centro de Investigaciones Geológicas. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Centro de Investigaciones Geológicas; ArgentinaFil: Spalletti, Luis Antonio. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata. Centro de Investigaciones Geológicas. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Centro de Investigaciones Geológicas; Argentina2015 Annual Convention and ExhibitionDenverEstados UnidosAmerican Association of Petroleum GeologistsAmerican Association of Petroleum Geologists2015info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/conferenceObjectExposiciónBookhttp://purl.org/coar/resource_type/c_5794info:ar-repo/semantics/documentoDeConferenciaapplication/pdfapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/234413Relationships between depositional processes, geochemical signature and seismic geometries in the Vaca Muerta Formation, Neuquén Basin, Argentina; 2015 Annual Convention and Exhibition; Denver; Estados Unidos; 2015; 1-1CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/https://www.searchanddiscovery.com/abstracts/html/2015/90216ace/abstracts/2104880.htmlinfo:eu-repo/semantics/altIdentifier/url/https://www.searchanddiscovery.com/abstracts/html/2015/90216ace/Internacionalinfo:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-03T10:09:03Zoai:ri.conicet.gov.ar:11336/234413instacron: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:34982025-09-03 10:09:03.348CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Relationships between depositional processes, geochemical signature and seismic geometries in the Vaca Muerta Formation, Neuquén Basin, Argentina
title Relationships between depositional processes, geochemical signature and seismic geometries in the Vaca Muerta Formation, Neuquén Basin, Argentina
spellingShingle Relationships between depositional processes, geochemical signature and seismic geometries in the Vaca Muerta Formation, Neuquén Basin, Argentina
Sagasti, Guillermina
Neuquén Basin
Geochemistry
Vaca Muerta Formation
Argentina
title_short Relationships between depositional processes, geochemical signature and seismic geometries in the Vaca Muerta Formation, Neuquén Basin, Argentina
title_full Relationships between depositional processes, geochemical signature and seismic geometries in the Vaca Muerta Formation, Neuquén Basin, Argentina
title_fullStr Relationships between depositional processes, geochemical signature and seismic geometries in the Vaca Muerta Formation, Neuquén Basin, Argentina
title_full_unstemmed Relationships between depositional processes, geochemical signature and seismic geometries in the Vaca Muerta Formation, Neuquén Basin, Argentina
title_sort Relationships between depositional processes, geochemical signature and seismic geometries in the Vaca Muerta Formation, Neuquén Basin, Argentina
dc.creator.none.fl_str_mv Sagasti, Guillermina
Remirez, Mariano Nicolas
Spalletti, Luis Antonio
author Sagasti, Guillermina
author_facet Sagasti, Guillermina
Remirez, Mariano Nicolas
Spalletti, Luis Antonio
author_role author
author2 Remirez, Mariano Nicolas
Spalletti, Luis Antonio
author2_role author
author
dc.subject.none.fl_str_mv Neuquén Basin
Geochemistry
Vaca Muerta Formation
Argentina
topic Neuquén Basin
Geochemistry
Vaca Muerta Formation
Argentina
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv The Upper Jurassic-Lower Cretaceous Vaca Muerta Formation (VMF) in the NeuquénBasin (Argentina) has recently emerged as the main shale oil/gas producer outside USA. The VMF is an extensive world-class hydrocarbon source rock with a prospective area in the order of 30.000 km2. The unit is part of a mixed clastic-carbonate succession deposited in a distally-steepened ramp, characterized by the development of northwest prograding clinoforms. In order to investigate possible relationships between depositional processes, geochemical signature, and geometries, which ultimately impact reservoir production, an integrated study involving inorganic geochemistry, core characterization, and seismic interpretation was conducted along a dip-oriented transect (ca. 25 km) in the center of the Neuquén Basin. The basinal facies are primarily composed of laminated mudstones with the highest content of redoxsensitive elements (V, Mo, Cr, Co, Ni, Zn) depicting sub-horizontal parallel reflections. Toe-of-slope facies comprises mainly laminated and bioturbated mudstones showing a decrease in the amount of redoxsensitive elements coupled with an increment in elements indicative of siliciclastic sedimentation (Si, Al,K, Zr, Ti) and availability of nutrients (Ba, P). Finally, upper slope and roll-over facies involve bioturbatedmudstones and mudstones with benthonic foraminifera and are characterized by a relative decrease in elements indicative of siliciclastic sedimentation along with an increase in elements with carbonate affinity (Ca, Sc, P). These results suggest a genetic relationship between inorganic geochemical signature and depositional processes along the clinoform, thus providing and additional proxy to evaluate shale reservoirs particularly in the absence of core and/or 3D seismic data.
Fil: Sagasti, Guillermina. Ypf Sociedad Anonima. Gerencia de Geociencias y Reservorios; Argentina
Fil: Remirez, Mariano Nicolas. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata. Centro de Investigaciones Geológicas. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Centro de Investigaciones Geológicas; Argentina
Fil: Spalletti, Luis Antonio. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata. Centro de Investigaciones Geológicas. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Centro de Investigaciones Geológicas; Argentina
2015 Annual Convention and Exhibition
Denver
Estados Unidos
American Association of Petroleum Geologists
description The Upper Jurassic-Lower Cretaceous Vaca Muerta Formation (VMF) in the NeuquénBasin (Argentina) has recently emerged as the main shale oil/gas producer outside USA. The VMF is an extensive world-class hydrocarbon source rock with a prospective area in the order of 30.000 km2. The unit is part of a mixed clastic-carbonate succession deposited in a distally-steepened ramp, characterized by the development of northwest prograding clinoforms. In order to investigate possible relationships between depositional processes, geochemical signature, and geometries, which ultimately impact reservoir production, an integrated study involving inorganic geochemistry, core characterization, and seismic interpretation was conducted along a dip-oriented transect (ca. 25 km) in the center of the Neuquén Basin. The basinal facies are primarily composed of laminated mudstones with the highest content of redoxsensitive elements (V, Mo, Cr, Co, Ni, Zn) depicting sub-horizontal parallel reflections. Toe-of-slope facies comprises mainly laminated and bioturbated mudstones showing a decrease in the amount of redoxsensitive elements coupled with an increment in elements indicative of siliciclastic sedimentation (Si, Al,K, Zr, Ti) and availability of nutrients (Ba, P). Finally, upper slope and roll-over facies involve bioturbatedmudstones and mudstones with benthonic foraminifera and are characterized by a relative decrease in elements indicative of siliciclastic sedimentation along with an increase in elements with carbonate affinity (Ca, Sc, P). These results suggest a genetic relationship between inorganic geochemical signature and depositional processes along the clinoform, thus providing and additional proxy to evaluate shale reservoirs particularly in the absence of core and/or 3D seismic data.
publishDate 2015
dc.date.none.fl_str_mv 2015
dc.type.none.fl_str_mv info:eu-repo/semantics/publishedVersion
info:eu-repo/semantics/conferenceObject
Exposición
Book
http://purl.org/coar/resource_type/c_5794
info:ar-repo/semantics/documentoDeConferencia
status_str publishedVersion
format conferenceObject
dc.identifier.none.fl_str_mv http://hdl.handle.net/11336/234413
Relationships between depositional processes, geochemical signature and seismic geometries in the Vaca Muerta Formation, Neuquén Basin, Argentina; 2015 Annual Convention and Exhibition; Denver; Estados Unidos; 2015; 1-1
CONICET Digital
CONICET
url http://hdl.handle.net/11336/234413
identifier_str_mv Relationships between depositional processes, geochemical signature and seismic geometries in the Vaca Muerta Formation, Neuquén Basin, Argentina; 2015 Annual Convention and Exhibition; Denver; Estados Unidos; 2015; 1-1
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://www.searchanddiscovery.com/abstracts/html/2015/90216ace/abstracts/2104880.html
info:eu-repo/semantics/altIdentifier/url/https://www.searchanddiscovery.com/abstracts/html/2015/90216ace/
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
application/pdf
dc.coverage.none.fl_str_mv Internacional
dc.publisher.none.fl_str_mv American Association of Petroleum Geologists
publisher.none.fl_str_mv American Association of Petroleum Geologists
dc.source.none.fl_str_mv reponame:CONICET Digital (CONICET)
instname:Consejo Nacional de Investigaciones Científicas y Técnicas
reponame_str CONICET Digital (CONICET)
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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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