3D reconstruction of syn-tectonic strata deposited during the inversion of salt-related structures

The Llert syncline is located in the South-central Pyrenees, between the eastern termination of the EW-trending Cotiella Basin and the north-western limb of the NS-trending Turbón-Serrado fold system. The Cotiella Basin is an inverted upper Coniacian-lower Santonian salt-floored post-rift extensiona...

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Autores: Ramos Ordoño, Adrià|||0000-0001-8224-9165, Lopez-Mir, Berta|||0000-0002-0617-7793, Wilson, Elisabeth P., Martínez Granado, Pablo|||0000-0002-1940-6647, Muñoz, Josep Anton|||0000-0003-0740-879X
Tipo de recurso: artículo
Fecha de publicación:2020
País:España
Institución:Universitat Autònoma de Barcelona
Repositorio:Dipòsit Digital de Documents de la UAB
Idioma:inglés
OAI Identifier:oai:ddd.uab.cat:235167
Acceso en línea:https://ddd.uab.cat/record/235167
https://dx.doi.org/urn:doi:10.1344/GeologicaActa2020.18.20
Access Level:acceso abierto
Palabra clave:3d reconstruction
Cotiella basin
Detachment anticlines
Salt tectonics
Tectonic inversion
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spelling 3D reconstruction of syn-tectonic strata deposited during the inversion of salt-related structuresinsights from the Llert syncline (South-central Pyrenees)Ramos Ordoño, Adrià|||0000-0001-8224-9165Lopez-Mir, Berta|||0000-0002-0617-7793Wilson, Elisabeth P.Martínez Granado, Pablo|||0000-0002-1940-6647Muñoz, Josep Anton|||0000-0003-0740-879X3d reconstructionCotiella basinDetachment anticlinesSalt tectonicsTectonic inversionThe Llert syncline is located in the South-central Pyrenees, between the eastern termination of the EW-trending Cotiella Basin and the north-western limb of the NS-trending Turbón-Serrado fold system. The Cotiella Basin is an inverted upper Coniacian-lower Santonian salt-floored post-rift extensional basin developed along the northern Iberian rift system. The Turbón-Serrado fold system consists of upper Santonian - Maastrichtian contractional salt-cored anticlines developed along an inverted transfer zone of the Pyrenean rift system. Based on field research, this paper presents a 3D reconstruction of the Llert syncline in order to further constrain the transition between these oblique salt-related structures. Our results suggest that the evolution of the Llert syncline was mainly controlled by tectonic shortening related to the tectonic inversion of the Cotiella Basin synchronously to the growth of the Turbón-Serrado detachment anticline, and by the pre-compressional structural framework of the Pyrenean rift system. Our contribution provides new insight into the geometric and kinematic relationships of structures developed during the inversion of passive margins involving salt. 22020-01-0120202020-01-01Articlehttp://purl.org/coar/resource_type/c_6501VoRhttp://purl.org/coar/version/c_970fb48d4fbd8a85info:eu-repo/semantics/articleapplication/pdfhttps://ddd.uab.cat/record/235167https://dx.doi.org/urn:doi:10.1344/GeologicaActa2020.18.20reponame:Dipòsit Digital de Documents de la UABinstname:Universitat Autònoma de BarcelonaInglésengopen accesshttp://purl.org/coar/access_right/c_abf2Aquest document està subjecte a una llicència d'ús Creative Commons. Es permet la reproducció total o parcial, la distribució, la comunicació pública de l'obra i la creació d'obres derivades, sempre i quan aquestes es distribueixin sota la mateixa llicència que regula l'obra original i es reconegui l'autoria.https://creativecommons.org/licenses/by-sa/4.0/info:eu-repo/semantics/openAccessoai:ddd.uab.cat:2351672026-06-06T12:50:31Z
dc.title.none.fl_str_mv 3D reconstruction of syn-tectonic strata deposited during the inversion of salt-related structures
insights from the Llert syncline (South-central Pyrenees)
title 3D reconstruction of syn-tectonic strata deposited during the inversion of salt-related structures
spellingShingle 3D reconstruction of syn-tectonic strata deposited during the inversion of salt-related structures
Ramos Ordoño, Adrià|||0000-0001-8224-9165
3d reconstruction
Cotiella basin
Detachment anticlines
Salt tectonics
Tectonic inversion
title_short 3D reconstruction of syn-tectonic strata deposited during the inversion of salt-related structures
title_full 3D reconstruction of syn-tectonic strata deposited during the inversion of salt-related structures
title_fullStr 3D reconstruction of syn-tectonic strata deposited during the inversion of salt-related structures
title_full_unstemmed 3D reconstruction of syn-tectonic strata deposited during the inversion of salt-related structures
title_sort 3D reconstruction of syn-tectonic strata deposited during the inversion of salt-related structures
dc.creator.none.fl_str_mv Ramos Ordoño, Adrià|||0000-0001-8224-9165
Lopez-Mir, Berta|||0000-0002-0617-7793
Wilson, Elisabeth P.
Martínez Granado, Pablo|||0000-0002-1940-6647
Muñoz, Josep Anton|||0000-0003-0740-879X
author Ramos Ordoño, Adrià|||0000-0001-8224-9165
author_facet Ramos Ordoño, Adrià|||0000-0001-8224-9165
Lopez-Mir, Berta|||0000-0002-0617-7793
Wilson, Elisabeth P.
Martínez Granado, Pablo|||0000-0002-1940-6647
Muñoz, Josep Anton|||0000-0003-0740-879X
author_role author
author2 Lopez-Mir, Berta|||0000-0002-0617-7793
Wilson, Elisabeth P.
Martínez Granado, Pablo|||0000-0002-1940-6647
Muñoz, Josep Anton|||0000-0003-0740-879X
author2_role author
author
author
author
dc.subject.none.fl_str_mv 3d reconstruction
Cotiella basin
Detachment anticlines
Salt tectonics
Tectonic inversion
topic 3d reconstruction
Cotiella basin
Detachment anticlines
Salt tectonics
Tectonic inversion
description The Llert syncline is located in the South-central Pyrenees, between the eastern termination of the EW-trending Cotiella Basin and the north-western limb of the NS-trending Turbón-Serrado fold system. The Cotiella Basin is an inverted upper Coniacian-lower Santonian salt-floored post-rift extensional basin developed along the northern Iberian rift system. The Turbón-Serrado fold system consists of upper Santonian - Maastrichtian contractional salt-cored anticlines developed along an inverted transfer zone of the Pyrenean rift system. Based on field research, this paper presents a 3D reconstruction of the Llert syncline in order to further constrain the transition between these oblique salt-related structures. Our results suggest that the evolution of the Llert syncline was mainly controlled by tectonic shortening related to the tectonic inversion of the Cotiella Basin synchronously to the growth of the Turbón-Serrado detachment anticline, and by the pre-compressional structural framework of the Pyrenean rift system. Our contribution provides new insight into the geometric and kinematic relationships of structures developed during the inversion of passive margins involving salt.
publishDate 2020
dc.date.none.fl_str_mv 2
2020-01-01
2020
2020-01-01
dc.type.none.fl_str_mv Article
http://purl.org/coar/resource_type/c_6501
VoR
http://purl.org/coar/version/c_970fb48d4fbd8a85
dc.type.openaire.fl_str_mv info:eu-repo/semantics/article
format article
dc.identifier.none.fl_str_mv https://ddd.uab.cat/record/235167
https://dx.doi.org/urn:doi:10.1344/GeologicaActa2020.18.20
url https://ddd.uab.cat/record/235167
https://dx.doi.org/urn:doi:10.1344/GeologicaActa2020.18.20
dc.language.none.fl_str_mv Inglés
eng
language_invalid_str_mv Inglés
language eng
dc.rights.none.fl_str_mv open access
http://purl.org/coar/access_right/c_abf2
https://creativecommons.org/licenses/by-sa/4.0/
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
https://creativecommons.org/licenses/by-sa/4.0/
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv application/pdf
dc.source.none.fl_str_mv reponame:Dipòsit Digital de Documents de la UAB
instname:Universitat Autònoma de Barcelona
instname_str Universitat Autònoma de Barcelona
reponame_str Dipòsit Digital de Documents de la UAB
collection Dipòsit Digital de Documents de la UAB
repository.name.fl_str_mv
repository.mail.fl_str_mv
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