Estudio comparado de la evolución e inversión de distintas cuencas mesozoicas de la Placa Ibérica

The marginal zones of the Maestrazgo Basin (Las Parras and Galve basins) and the Algarve Basin show a similar evolution during basin formation (mainly Jurassic and Early Cretaceous) and inversion (Oligocene-Early Miocene). Common features between the two basins are the control of sedimentation durin...

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Autores: Casas Sainz, Antonio, Cortés Gracia, A. L., Liesa, Carlos L., Soria, Ana Rosa, Terrinha, P., Kullberg, J. C., Rocha, R. da
Tipo de recurso: artículo
Fecha de publicación:1997
País:España
Institución:Universidad de Huelva (UHU)
Repositorio:Arias Montano. Repositorio Institucional de la Universidad de Huelva
Idioma:español
OAI Identifier:oai:ariasmontano.uhu.es:10272/10237
Acceso en línea:http://hdl.handle.net/10272/10237
Access Level:acceso abierto
Palabra clave:Sedimentary basin
Basin inversion
Basement fault
Mesozoic
Tertiary
Iberian plate
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spelling Estudio comparado de la evolución e inversión de distintas cuencas mesozoicas de la Placa IbéricaComparative study ofthe evolution and inversión ofseveral Mesozoic basins within thè Iberian píateCasas Sainz, AntonioCortés Gracia, A. L.Liesa, Carlos L.Soria, Ana RosaTerrinha, P.Kullberg, J. C.Rocha, R. daSedimentary basinBasin inversionBasement faultMesozoicTertiaryIberian plateThe marginal zones of the Maestrazgo Basin (Las Parras and Galve basins) and the Algarve Basin show a similar evolution during basin formation (mainly Jurassic and Early Cretaceous) and inversion (Oligocene-Early Miocene). Common features between the two basins are the control of sedimentation during extension by basement normal and transfer faults (NW-SE and NE-SW) and the complete inversion during the Tertiary accomodated by basement-involved E-W thrusts, preserving the extensional geometry with non-reactivated normal faults at the thrusts hanging-walls. Extensional structures in the Las Parras and Calve basins are consistent with a roughly N-S oriented extension (locally NE-SW and NW-SE, perpendicular to the main normal faults). Thrusts show an overall E-W direction compatible with a near N-S shortening between the Late Eocene and the Early Miocene. Extension in the Algarve Basin was accomodated by ENE-WSW to NE-SW late Variscan faults; NW-SE transfer faults dipping to the Northeast also accomodated some extension and divided the area into sub-basins. Inversion in the Algarve Basin pre-dated deposition ofthe Miocene sediments and was accomodated by S- to S-SE directed thrusts, which cross-cut the main extensional faultsSociedad Geológica de España19971997-01-0119971997-01-01journal articlehttp://purl.org/coar/resource_type/c_6501info:eu-repo/semantics/articleapplication/pdfhttp://hdl.handle.net/10272/10237reponame:Arias Montano. Repositorio Institucional de la Universidad de Huelvainstname:Universidad de Huelva (UHU)Españolspaopen accesshttp://purl.org/coar/access_right/c_abf2Atribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/info:eu-repo/semantics/openAccessoai:ariasmontano.uhu.es:10272/102372026-06-02T14:58:11Z
dc.title.none.fl_str_mv Estudio comparado de la evolución e inversión de distintas cuencas mesozoicas de la Placa Ibérica
Comparative study ofthe evolution and inversión ofseveral Mesozoic basins within thè Iberian píate
title Estudio comparado de la evolución e inversión de distintas cuencas mesozoicas de la Placa Ibérica
spellingShingle Estudio comparado de la evolución e inversión de distintas cuencas mesozoicas de la Placa Ibérica
Casas Sainz, Antonio
Sedimentary basin
Basin inversion
Basement fault
Mesozoic
Tertiary
Iberian plate
title_short Estudio comparado de la evolución e inversión de distintas cuencas mesozoicas de la Placa Ibérica
title_full Estudio comparado de la evolución e inversión de distintas cuencas mesozoicas de la Placa Ibérica
title_fullStr Estudio comparado de la evolución e inversión de distintas cuencas mesozoicas de la Placa Ibérica
title_full_unstemmed Estudio comparado de la evolución e inversión de distintas cuencas mesozoicas de la Placa Ibérica
title_sort Estudio comparado de la evolución e inversión de distintas cuencas mesozoicas de la Placa Ibérica
dc.creator.none.fl_str_mv Casas Sainz, Antonio
Cortés Gracia, A. L.
Liesa, Carlos L.
Soria, Ana Rosa
Terrinha, P.
Kullberg, J. C.
Rocha, R. da
author Casas Sainz, Antonio
author_facet Casas Sainz, Antonio
Cortés Gracia, A. L.
Liesa, Carlos L.
Soria, Ana Rosa
Terrinha, P.
Kullberg, J. C.
Rocha, R. da
author_role author
author2 Cortés Gracia, A. L.
Liesa, Carlos L.
Soria, Ana Rosa
Terrinha, P.
Kullberg, J. C.
Rocha, R. da
author2_role author
author
author
author
author
author
dc.contributor.none.fl_str_mv
dc.subject.none.fl_str_mv Sedimentary basin
Basin inversion
Basement fault
Mesozoic
Tertiary
Iberian plate
topic Sedimentary basin
Basin inversion
Basement fault
Mesozoic
Tertiary
Iberian plate
description The marginal zones of the Maestrazgo Basin (Las Parras and Galve basins) and the Algarve Basin show a similar evolution during basin formation (mainly Jurassic and Early Cretaceous) and inversion (Oligocene-Early Miocene). Common features between the two basins are the control of sedimentation during extension by basement normal and transfer faults (NW-SE and NE-SW) and the complete inversion during the Tertiary accomodated by basement-involved E-W thrusts, preserving the extensional geometry with non-reactivated normal faults at the thrusts hanging-walls. Extensional structures in the Las Parras and Calve basins are consistent with a roughly N-S oriented extension (locally NE-SW and NW-SE, perpendicular to the main normal faults). Thrusts show an overall E-W direction compatible with a near N-S shortening between the Late Eocene and the Early Miocene. Extension in the Algarve Basin was accomodated by ENE-WSW to NE-SW late Variscan faults; NW-SE transfer faults dipping to the Northeast also accomodated some extension and divided the area into sub-basins. Inversion in the Algarve Basin pre-dated deposition ofthe Miocene sediments and was accomodated by S- to S-SE directed thrusts, which cross-cut the main extensional faults
publishDate 1997
dc.date.none.fl_str_mv 1997
1997-01-01
1997
1997-01-01
dc.type.none.fl_str_mv journal article
http://purl.org/coar/resource_type/c_6501
dc.type.openaire.fl_str_mv info:eu-repo/semantics/article
format article
dc.identifier.none.fl_str_mv http://hdl.handle.net/10272/10237
url http://hdl.handle.net/10272/10237
dc.language.none.fl_str_mv Español
spa
language_invalid_str_mv Español
language spa
dc.rights.none.fl_str_mv open access
http://purl.org/coar/access_right/c_abf2
Atribución-NoComercial-SinDerivadas 3.0 España
http://creativecommons.org/licenses/by-nc-nd/3.0/es/
dc.rights.openaire.fl_str_mv info:eu-repo/semantics/openAccess
rights_invalid_str_mv open access
http://purl.org/coar/access_right/c_abf2
Atribución-NoComercial-SinDerivadas 3.0 España
http://creativecommons.org/licenses/by-nc-nd/3.0/es/
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv application/pdf
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:Arias Montano. Repositorio Institucional de la Universidad de Huelva
instname:Universidad de Huelva (UHU)
instname_str Universidad de Huelva (UHU)
reponame_str Arias Montano. Repositorio Institucional de la Universidad de Huelva
collection Arias Montano. Repositorio Institucional de la Universidad de Huelva
repository.name.fl_str_mv
repository.mail.fl_str_mv
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score 15,81155

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