Dating the northern deposits of the Ebro foreland basin; implications for the kinematics of the SW Pyrenean front

Dating the sedimentary infill of the northern margin of the Ebro foreland basin informs about the orogen-basin evolution. A magnetostratigraphic section of ~5 km-thick combines new magnetostratigraphic results from the syntectonic alluvial ncastillo Fm (Upper Oligocene-Lower Miocene, 1 km-thick, the...

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Autores: Oliva-Urcia, Belén, Beamud Amorós, Elisabet, Arenas, Concha, Pueyo, Emilio, Garcés Crespo, Miguel, Soto Marín, Ruth, Valero Montesa, Luis, Pérez-Rivarés, Javier
Tipo de recurso: artículo
Estado:Versión aceptada para publicación
Fecha de publicación:2019
País:España
Institución:Universidad de Barcelona
Repositorio:Dipòsit Digital de la UB
OAI Identifier:oai:diposit.ub.edu:2445/134326
Acceso en línea:https://hdl.handle.net/2445/134326
Access Level:acceso abierto
Palabra clave:Sedimentologia
Magnetoestratigrafia
Cinemàtica
Ebre, Conca de l'
Sedimentology
Magnetostratigraphy
Kinematics
Ebro River Watershead
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spelling Dating the northern deposits of the Ebro foreland basin; implications for the kinematics of the SW Pyrenean frontOliva-Urcia, BelénBeamud Amorós, ElisabetArenas, ConchaPueyo, EmilioGarcés Crespo, MiguelSoto Marín, RuthValero Montesa, LuisPérez-Rivarés, JavierSedimentologiaMagnetoestratigrafiaCinemàticaEbre, Conca de l'SedimentologyMagnetostratigraphyKinematicsEbro River WatersheadDating the sedimentary infill of the northern margin of the Ebro foreland basin informs about the orogen-basin evolution. A magnetostratigraphic section of ~5 km-thick combines new magnetostratigraphic results from the syntectonic alluvial ncastillo Fm (Upper Oligocene-Lower Miocene, 1 km-thick, the Fuencalderas section) with previous (3.3 km-thick) and new (0.7 km thick) magnetostratigraphic data from the underlying fluvial Campodarbe Fm (Luesia and San Marzal sections, Eocene-Oligocene). This composite section allows dating the entire basin infill in this sector, therefore bracketing the timing of the deformation in the southern margin of the Pyrenees after considering previous kinematic studies. Deformation recorded by the continental deposits spans from syn-Gavarnie nappe activity (Broto and Fiscal basement thrust sheets) from 31.3 to 24.55 Ma, Rupelian-Chattian (Oligocene) to the syn-Guarga thrust activity, from 24.55 to 21.2 Ma Chattian-Aquitanian (Oligocene-Miocene). The Accumulation rates vary from ca. 22 to ca. 39 cm/kyr between the genetic stratigraphic units in the Uncastillo Fm through the section. These rates are close to those of the underlying deposits of the Campodarbe Fm (average of ca. 36 cm/kyr). Deformation for the latest Pyrenean front (syn-Guarga thrust) is younger than previously assigned in ~ 5.4. ~1.5 and ~1.1 Myr of the beginning of the Punta Común thrust sheet (from 29.4 Ma to 24 Ma), Lower Riglos thrust sheet system (from 24 to 22.5 Ma) and the Upper Riglos thrust system (22.5 to 21.4 Ma) respectively. Other significant changes in accumulation rate and its derivative also indicate variations in the tectonic activity ca. 33 and 28 Ma. Tilt variations in the Uncastillo Fm also record the tectonic activity with 40º variations of the Punta Común thrust sheet at ca. 20º with the Upper Riglos thrust sheet.Elsevier B.V.2019info:eu-repo/semantics/articleinfo:eu-repo/semantics/acceptedVersionapplication/pdfhttps://hdl.handle.net/2445/134326Articles publicats en revistes (Dinàmica de la Terra i l'Oceà)reponame:Dipòsit Digital de la UBinstname:Universidad de BarcelonaInglésVersió postprint del document publicat a: https://doi.org/10.1016/j.tecto.2019.05.007Tectonophysics, 2019, vol. 765, p. 11-34https://doi.org/10.1016/j.tecto.2019.05.007cc-by-nc-nd (c) Elsevier B.V., 2019http://creativecommons.org/licenses/by-nc-nd/3.0/esinfo:eu-repo/semantics/openAccessoai:diposit.ub.edu:2445/1343262026-05-27T06:46:51Z
dc.title.none.fl_str_mv Dating the northern deposits of the Ebro foreland basin; implications for the kinematics of the SW Pyrenean front
title Dating the northern deposits of the Ebro foreland basin; implications for the kinematics of the SW Pyrenean front
spellingShingle Dating the northern deposits of the Ebro foreland basin; implications for the kinematics of the SW Pyrenean front
Oliva-Urcia, Belén
Sedimentologia
Magnetoestratigrafia
Cinemàtica
Ebre, Conca de l'
Sedimentology
Magnetostratigraphy
Kinematics
Ebro River Watershead
title_short Dating the northern deposits of the Ebro foreland basin; implications for the kinematics of the SW Pyrenean front
title_full Dating the northern deposits of the Ebro foreland basin; implications for the kinematics of the SW Pyrenean front
title_fullStr Dating the northern deposits of the Ebro foreland basin; implications for the kinematics of the SW Pyrenean front
title_full_unstemmed Dating the northern deposits of the Ebro foreland basin; implications for the kinematics of the SW Pyrenean front
title_sort Dating the northern deposits of the Ebro foreland basin; implications for the kinematics of the SW Pyrenean front
dc.creator.none.fl_str_mv Oliva-Urcia, Belén
Beamud Amorós, Elisabet
Arenas, Concha
Pueyo, Emilio
Garcés Crespo, Miguel
Soto Marín, Ruth
Valero Montesa, Luis
Pérez-Rivarés, Javier
author Oliva-Urcia, Belén
author_facet Oliva-Urcia, Belén
Beamud Amorós, Elisabet
Arenas, Concha
Pueyo, Emilio
Garcés Crespo, Miguel
Soto Marín, Ruth
Valero Montesa, Luis
Pérez-Rivarés, Javier
author_role author
author2 Beamud Amorós, Elisabet
Arenas, Concha
Pueyo, Emilio
Garcés Crespo, Miguel
Soto Marín, Ruth
Valero Montesa, Luis
Pérez-Rivarés, Javier
author2_role author
author
author
author
author
author
author
dc.subject.none.fl_str_mv Sedimentologia
Magnetoestratigrafia
Cinemàtica
Ebre, Conca de l'
Sedimentology
Magnetostratigraphy
Kinematics
Ebro River Watershead
topic Sedimentologia
Magnetoestratigrafia
Cinemàtica
Ebre, Conca de l'
Sedimentology
Magnetostratigraphy
Kinematics
Ebro River Watershead
description Dating the sedimentary infill of the northern margin of the Ebro foreland basin informs about the orogen-basin evolution. A magnetostratigraphic section of ~5 km-thick combines new magnetostratigraphic results from the syntectonic alluvial ncastillo Fm (Upper Oligocene-Lower Miocene, 1 km-thick, the Fuencalderas section) with previous (3.3 km-thick) and new (0.7 km thick) magnetostratigraphic data from the underlying fluvial Campodarbe Fm (Luesia and San Marzal sections, Eocene-Oligocene). This composite section allows dating the entire basin infill in this sector, therefore bracketing the timing of the deformation in the southern margin of the Pyrenees after considering previous kinematic studies. Deformation recorded by the continental deposits spans from syn-Gavarnie nappe activity (Broto and Fiscal basement thrust sheets) from 31.3 to 24.55 Ma, Rupelian-Chattian (Oligocene) to the syn-Guarga thrust activity, from 24.55 to 21.2 Ma Chattian-Aquitanian (Oligocene-Miocene). The Accumulation rates vary from ca. 22 to ca. 39 cm/kyr between the genetic stratigraphic units in the Uncastillo Fm through the section. These rates are close to those of the underlying deposits of the Campodarbe Fm (average of ca. 36 cm/kyr). Deformation for the latest Pyrenean front (syn-Guarga thrust) is younger than previously assigned in ~ 5.4. ~1.5 and ~1.1 Myr of the beginning of the Punta Común thrust sheet (from 29.4 Ma to 24 Ma), Lower Riglos thrust sheet system (from 24 to 22.5 Ma) and the Upper Riglos thrust system (22.5 to 21.4 Ma) respectively. Other significant changes in accumulation rate and its derivative also indicate variations in the tectonic activity ca. 33 and 28 Ma. Tilt variations in the Uncastillo Fm also record the tectonic activity with 40º variations of the Punta Común thrust sheet at ca. 20º with the Upper Riglos thrust sheet.
publishDate 2019
dc.date.none.fl_str_mv 2019
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/acceptedVersion
format article
status_str acceptedVersion
dc.identifier.none.fl_str_mv https://hdl.handle.net/2445/134326
url https://hdl.handle.net/2445/134326
dc.language.none.fl_str_mv Inglés
language_invalid_str_mv Inglés
dc.relation.none.fl_str_mv Versió postprint del document publicat a: https://doi.org/10.1016/j.tecto.2019.05.007
Tectonophysics, 2019, vol. 765, p. 11-34
https://doi.org/10.1016/j.tecto.2019.05.007
dc.rights.none.fl_str_mv cc-by-nc-nd (c) Elsevier B.V., 2019
http://creativecommons.org/licenses/by-nc-nd/3.0/es
info:eu-repo/semantics/openAccess
rights_invalid_str_mv cc-by-nc-nd (c) Elsevier B.V., 2019
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 Elsevier B.V.
publisher.none.fl_str_mv Elsevier B.V.
dc.source.none.fl_str_mv Articles publicats en revistes (Dinàmica de la Terra i l'Oceà)
reponame:Dipòsit Digital de la UB
instname:Universidad de Barcelona
instname_str Universidad de Barcelona
reponame_str Dipòsit Digital de la UB
collection Dipòsit Digital de la UB
repository.name.fl_str_mv
repository.mail.fl_str_mv
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