Basement structure of the Hontomín CO2 Geological storage facility (Burgos, Spain): integration of microgravity & 3D seismic reflection data

The structure of the Hontomín CO2 geological storage research facility has been addressed combining 3D seismic reflection data, borehole information and microgravity data. The integrated interpretation constrains the basement structural setting geometry and that of the sedimentary succession. The st...

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Autores: Andrés, Juvenal, Alcalde, Juan, Ayarza, P., Saura, Eduard, Marzán, Ignacio, Martí, David, Martínez Catalán, J. R., Carbonell, Ramón, Pérez-Estaún, Andrés, García Lobón, José Luis, Rubio Sánchez-Aguililla, Félix Manuel
Tipo de recurso: artículo
Estado:Versión publicada
Fecha de publicación:2016
País:España
Institución:Consejo Superior de Investigaciones Científicas (CSIC)
Repositorio:DIGITAL.CSIC. Repositorio Institucional del CSIC
OAI Identifier:oai:digital.csic.es:10261/148207
Acceso en línea:http://hdl.handle.net/10261/148207
Access Level:acceso abierto
Palabra clave:structural geology
Basement
Microgravity
Microgravimetría
sísmica 3D
Basamento
geología estructural
3D seismics
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spelling Basement structure of the Hontomín CO2 Geological storage facility (Burgos, Spain): integration of microgravity & 3D seismic reflection dataAndrés, JuvenalAlcalde, JuanAyarza, P.Saura, EduardMarzán, IgnacioMartí, DavidMartínez Catalán, J. R.Carbonell, RamónPérez-Estaún, AndrésGarcía Lobón, José LuisRubio Sánchez-Aguililla, Félix Manuelstructural geologyBasementMicrogravityMicrogravimetríasísmica 3DBasamentogeología estructural3D seismicsThe structure of the Hontomín CO2 geological storage research facility has been addressed combining 3D seismic reflection data, borehole information and microgravity data. The integrated interpretation constrains the basement structural setting geometry and that of the sedimentary succession. The study unravels the deep structure and topography of the basement and quantifies the thickness of the Triassic Keuper evaporites. We describe a half-graben setting filled with Keuper evaporites (up to 2000 m) forming an extensional forced fold. Three set of faults are identified with two main fault systems compartmentalizing the area into three differentiated blocks. These faults have been interpreted to be reactivated normal faults that have led to the formation of the Hontomín dome.The datasets in this work have been funded by Fundación Ciudad de la Energía (Spanish Government, www.ciuden.es) and by the European Union through the “European Energy Programme for Recovery” and the Compostilla OXYCFB300 project. Dr. Juan Alcalde is currently funded by NERC grant NE/M007251/1.Peer ReviewedSociedad Geológica de EspañaConsejo Superior de Investigaciones Científicas [https://ror.org/02gfc7t72]2017201720162017info:eu-repo/semantics/articlehttp://purl.org/coar/resource_type/c_6501Publisher's versioninfo:eu-repo/semantics/publishedVersionhttp://hdl.handle.net/10261/148207reponame:DIGITAL.CSIC. Repositorio Institucional del CSICinstname:Consejo Superior de Investigaciones Científicas (CSIC)InglésSíinfo:eu-repo/semantics/openAccessoai:digital.csic.es:10261/1482072026-05-22T06:33:51Z
dc.title.none.fl_str_mv Basement structure of the Hontomín CO2 Geological storage facility (Burgos, Spain): integration of microgravity & 3D seismic reflection data
title Basement structure of the Hontomín CO2 Geological storage facility (Burgos, Spain): integration of microgravity & 3D seismic reflection data
spellingShingle Basement structure of the Hontomín CO2 Geological storage facility (Burgos, Spain): integration of microgravity & 3D seismic reflection data
Andrés, Juvenal
structural geology
Basement
Microgravity
Microgravimetría
sísmica 3D
Basamento
geología estructural
3D seismics
title_short Basement structure of the Hontomín CO2 Geological storage facility (Burgos, Spain): integration of microgravity & 3D seismic reflection data
title_full Basement structure of the Hontomín CO2 Geological storage facility (Burgos, Spain): integration of microgravity & 3D seismic reflection data
title_fullStr Basement structure of the Hontomín CO2 Geological storage facility (Burgos, Spain): integration of microgravity & 3D seismic reflection data
title_full_unstemmed Basement structure of the Hontomín CO2 Geological storage facility (Burgos, Spain): integration of microgravity & 3D seismic reflection data
title_sort Basement structure of the Hontomín CO2 Geological storage facility (Burgos, Spain): integration of microgravity & 3D seismic reflection data
dc.creator.none.fl_str_mv Andrés, Juvenal
Alcalde, Juan
Ayarza, P.
Saura, Eduard
Marzán, Ignacio
Martí, David
Martínez Catalán, J. R.
Carbonell, Ramón
Pérez-Estaún, Andrés
García Lobón, José Luis
Rubio Sánchez-Aguililla, Félix Manuel
author Andrés, Juvenal
author_facet Andrés, Juvenal
Alcalde, Juan
Ayarza, P.
Saura, Eduard
Marzán, Ignacio
Martí, David
Martínez Catalán, J. R.
Carbonell, Ramón
Pérez-Estaún, Andrés
García Lobón, José Luis
Rubio Sánchez-Aguililla, Félix Manuel
author_role author
author2 Alcalde, Juan
Ayarza, P.
Saura, Eduard
Marzán, Ignacio
Martí, David
Martínez Catalán, J. R.
Carbonell, Ramón
Pérez-Estaún, Andrés
García Lobón, José Luis
Rubio Sánchez-Aguililla, Félix Manuel
author2_role author
author
author
author
author
author
author
author
author
author
dc.contributor.none.fl_str_mv Consejo Superior de Investigaciones Científicas [https://ror.org/02gfc7t72]
dc.subject.none.fl_str_mv structural geology
Basement
Microgravity
Microgravimetría
sísmica 3D
Basamento
geología estructural
3D seismics
topic structural geology
Basement
Microgravity
Microgravimetría
sísmica 3D
Basamento
geología estructural
3D seismics
description The structure of the Hontomín CO2 geological storage research facility has been addressed combining 3D seismic reflection data, borehole information and microgravity data. The integrated interpretation constrains the basement structural setting geometry and that of the sedimentary succession. The study unravels the deep structure and topography of the basement and quantifies the thickness of the Triassic Keuper evaporites. We describe a half-graben setting filled with Keuper evaporites (up to 2000 m) forming an extensional forced fold. Three set of faults are identified with two main fault systems compartmentalizing the area into three differentiated blocks. These faults have been interpreted to be reactivated normal faults that have led to the formation of the Hontomín dome.
publishDate 2016
dc.date.none.fl_str_mv 2016
2017
2017
2017
dc.type.none.fl_str_mv info:eu-repo/semantics/article
http://purl.org/coar/resource_type/c_6501
Publisher's version
info:eu-repo/semantics/publishedVersion
format article
status_str publishedVersion
dc.identifier.none.fl_str_mv http://hdl.handle.net/10261/148207
url http://hdl.handle.net/10261/148207
dc.language.none.fl_str_mv Inglés
language_invalid_str_mv Inglés
dc.relation.none.fl_str_mv
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
eu_rights_str_mv openAccess
dc.publisher.none.fl_str_mv Sociedad Geológica de España
publisher.none.fl_str_mv Sociedad Geológica de España
dc.source.none.fl_str_mv reponame:DIGITAL.CSIC. Repositorio Institucional del CSIC
instname:Consejo Superior de Investigaciones Científicas (CSIC)
instname_str Consejo Superior de Investigaciones Científicas (CSIC)
reponame_str DIGITAL.CSIC. Repositorio Institucional del CSIC
collection DIGITAL.CSIC. Repositorio Institucional del CSIC
repository.name.fl_str_mv
repository.mail.fl_str_mv
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score 15,811543