Climatic vs. tectonic signals in a continental extensional basin (Teruel, NE Spain) from stable isotope (δ18O) and sequence stratigraphical evolution

Alluvial fans and shallow carbonate lakes interfered in the Teruel half-graben during the Late Miocene–Pliocene. Tectonic influence is recorded in alluvial and lacustrine–palustrine successions, with long-term climate changes being recorded in detail in the isotopic signatures of carbonates. Episode...

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Autores: Ezquerro Ruiz, Lope, Luzón Aguado, Aránzazu, Navarro, Marta, Liesa, Carlos L., Simón, J.L.
Tipo de recurso: artículo
Fecha de publicación:2014
País:España
Institución:Universidad Complutense de Madrid (UCM)
Repositorio:Docta Complutense
Idioma:inglés
OAI Identifier:oai:docta.ucm.es:20.500.14352/116437
Acceso en línea:https://hdl.handle.net/20.500.14352/116437
Access Level:acceso abierto
Palabra clave:551.78(460.226)
Geología estratigráfica
2506.19 Estratigrafía
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spelling Climatic vs. tectonic signals in a continental extensional basin (Teruel, NE Spain) from stable isotope (δ18O) and sequence stratigraphical evolutionEzquerro Ruiz, LopeLuzón Aguado, AránzazuNavarro, MartaLiesa, Carlos L.Simón, J.L.551.78(460.226)Geología estratigráfica2506.19 EstratigrafíaAlluvial fans and shallow carbonate lakes interfered in the Teruel half-graben during the Late Miocene–Pliocene. Tectonic influence is recorded in alluvial and lacustrine–palustrine successions, with long-term climate changes being recorded in detail in the isotopic signatures of carbonates. Episodes of tectonic activity induced alluvial fan progradation and lake retraction in the whole basin. Three lacustrine stages have been identified, which support the idea that climate also exerted an important control on sedimentation. The transition between stages 1 and 2 occurred during a tectonically calm episode due to an increase in aridity in the Early Turolian; small fans with source areas next to the lake margin prograded, inducing lake-shore retraction. The transition from stage 2 to 3 was caused by the superimposition of increasing tectonic activity and aridity effects. Our study demonstrates that discrimination of allogenic factors controlling sedimentation in continental closed basins is possible using sequence stratigraphy in combination with other techniques such as geochemistry of carbonates.WileyUniversidad Complutense de Madrid20142014-01-0120142014-01-01journal articlehttp://purl.org/coar/resource_type/c_6501Phttp://purl.org/coar/version/c_fa2ee174bc00049finfo:eu-repo/semantics/articleapplication/pdfhttps://hdl.handle.net/20.500.14352/116437reponame:Docta Complutenseinstname:Universidad Complutense de Madrid (UCM)Inglésengopen accesshttp://purl.org/coar/access_right/c_abf2Attribution-NonCommercial-NoDerivatives 4.0 Internationalhttp://creativecommons.org/licenses/by-nc-nd/4.0/info:eu-repo/semantics/openAccessoai:docta.ucm.es:20.500.14352/1164372026-06-02T12:44:21Z
dc.title.none.fl_str_mv Climatic vs. tectonic signals in a continental extensional basin (Teruel, NE Spain) from stable isotope (δ18O) and sequence stratigraphical evolution
title Climatic vs. tectonic signals in a continental extensional basin (Teruel, NE Spain) from stable isotope (δ18O) and sequence stratigraphical evolution
spellingShingle Climatic vs. tectonic signals in a continental extensional basin (Teruel, NE Spain) from stable isotope (δ18O) and sequence stratigraphical evolution
Ezquerro Ruiz, Lope
551.78(460.226)
Geología estratigráfica
2506.19 Estratigrafía
title_short Climatic vs. tectonic signals in a continental extensional basin (Teruel, NE Spain) from stable isotope (δ18O) and sequence stratigraphical evolution
title_full Climatic vs. tectonic signals in a continental extensional basin (Teruel, NE Spain) from stable isotope (δ18O) and sequence stratigraphical evolution
title_fullStr Climatic vs. tectonic signals in a continental extensional basin (Teruel, NE Spain) from stable isotope (δ18O) and sequence stratigraphical evolution
title_full_unstemmed Climatic vs. tectonic signals in a continental extensional basin (Teruel, NE Spain) from stable isotope (δ18O) and sequence stratigraphical evolution
title_sort Climatic vs. tectonic signals in a continental extensional basin (Teruel, NE Spain) from stable isotope (δ18O) and sequence stratigraphical evolution
dc.creator.none.fl_str_mv Ezquerro Ruiz, Lope
Luzón Aguado, Aránzazu
Navarro, Marta
Liesa, Carlos L.
Simón, J.L.
author Ezquerro Ruiz, Lope
author_facet Ezquerro Ruiz, Lope
Luzón Aguado, Aránzazu
Navarro, Marta
Liesa, Carlos L.
Simón, J.L.
author_role author
author2 Luzón Aguado, Aránzazu
Navarro, Marta
Liesa, Carlos L.
Simón, J.L.
author2_role author
author
author
author
dc.contributor.none.fl_str_mv Universidad Complutense de Madrid
dc.subject.none.fl_str_mv 551.78(460.226)
Geología estratigráfica
2506.19 Estratigrafía
topic 551.78(460.226)
Geología estratigráfica
2506.19 Estratigrafía
description Alluvial fans and shallow carbonate lakes interfered in the Teruel half-graben during the Late Miocene–Pliocene. Tectonic influence is recorded in alluvial and lacustrine–palustrine successions, with long-term climate changes being recorded in detail in the isotopic signatures of carbonates. Episodes of tectonic activity induced alluvial fan progradation and lake retraction in the whole basin. Three lacustrine stages have been identified, which support the idea that climate also exerted an important control on sedimentation. The transition between stages 1 and 2 occurred during a tectonically calm episode due to an increase in aridity in the Early Turolian; small fans with source areas next to the lake margin prograded, inducing lake-shore retraction. The transition from stage 2 to 3 was caused by the superimposition of increasing tectonic activity and aridity effects. Our study demonstrates that discrimination of allogenic factors controlling sedimentation in continental closed basins is possible using sequence stratigraphy in combination with other techniques such as geochemistry of carbonates.
publishDate 2014
dc.date.none.fl_str_mv 2014
2014-01-01
2014
2014-01-01
dc.type.none.fl_str_mv journal article
http://purl.org/coar/resource_type/c_6501
P
http://purl.org/coar/version/c_fa2ee174bc00049f
dc.type.openaire.fl_str_mv info:eu-repo/semantics/article
format article
dc.identifier.none.fl_str_mv https://hdl.handle.net/20.500.14352/116437
url https://hdl.handle.net/20.500.14352/116437
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
Attribution-NonCommercial-NoDerivatives 4.0 International
http://creativecommons.org/licenses/by-nc-nd/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
Attribution-NonCommercial-NoDerivatives 4.0 International
http://creativecommons.org/licenses/by-nc-nd/4.0/
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv application/pdf
dc.publisher.none.fl_str_mv Wiley
publisher.none.fl_str_mv Wiley
dc.source.none.fl_str_mv reponame:Docta Complutense
instname:Universidad Complutense de Madrid (UCM)
instname_str Universidad Complutense de Madrid (UCM)
reponame_str Docta Complutense
collection Docta Complutense
repository.name.fl_str_mv
repository.mail.fl_str_mv
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score 15,808905

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