Late Quaternary morpho-stratigraphic record of diapir rise in the Cardona salt extrusion, NE Spain. Halokinetic sequences, raised terraces and uplift rates

Active diapirism has received very limited attention from the geomorphological and Quaternary Science perspective, despite the role played by this ground deformation process in the development of landforms and sedimentary environments, and the important practical implications associated with mobile...

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Autores: Pérez Villar, Guillermo, Gutiérrez Santolalla, Francisco, Zarroca, Mario, Roqué i Pau, Carles, Benito-Calvo, Alfonso, Menció i Domingo, Anna
Formato: artículo
Estado:Versión publicada
Fecha de publicación:2024
País:España
Recursos:Varias* (Consorci de Biblioteques Universitáries de Catalunya, Centre de Serveis Científics i Acadèmics de Catalunya)
Repositorio:Recercat. Dipósit de la Recerca de Catalunya
OAI Identifier:oai:recercat.cat:10256/25395
Acesso em linha:http://hdl.handle.net/10256/25395
Access Level:acceso abierto
Palavra-chave:Diapirs -- Catalunya -- Cardona
Diapirs -- Catalonia -- Cardona
Estratigrafia -- Quaternari
Geology, Stratigraphic -- Quaternary
Salines (Geologia) -- Catalunya -- Cardona
Salt pans (Geology) -- Catalonia -- Cardona
Jaciments salins -- Catalunya -- Cardona
Salt deposits -- Catalonia -- Cardona
Radiocarboni, Mètode del
Radiocarbon dating
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spelling Late Quaternary morpho-stratigraphic record of diapir rise in the Cardona salt extrusion, NE Spain. Halokinetic sequences, raised terraces and uplift ratesPérez Villar, GuillermoGutiérrez Santolalla, FranciscoZarroca, MarioRoqué i Pau, CarlesBenito-Calvo, AlfonsoMenció i Domingo, AnnaDiapirs -- Catalunya -- CardonaDiapirs -- Catalonia -- CardonaEstratigrafia -- QuaternariGeology, Stratigraphic -- QuaternarySalines (Geologia) -- Catalunya -- CardonaSalt pans (Geology) -- Catalonia -- CardonaJaciments salins -- Catalunya -- CardonaSalt deposits -- Catalonia -- CardonaRadiocarboni, Mètode delRadiocarbon datingActive diapirism has received very limited attention from the geomorphological and Quaternary Science perspective, despite the role played by this ground deformation process in the development of landforms and sedimentary environments, and the important practical implications associated with mobile salt structures (e,g., mining, hydrocarbon production, geostorage). The Cardona salt extrusion (NE Spain) was initiated in late Quaternary times from the post-shortening unroofing of the crest of a salt anticline by the entrenchment of the transverse Cardener River. Detailed mapping, outcrop analysis, geophysical data and trenching indicate that the diapir-flanking deposits show halokinetic complexes comprising two types of morpho-stratigraphic units: (1) an older flap of coarse-grained drapefolded colluvial deposits; and (2) younger lacustrine and fluvial deposits in peripheral depressions confined between the upturned colluvial flaps and the country rock slope. These synkinematic units record an overall relief inversion and correspond to the so-called wedge and hook halokinetic sequences, recording ratios between diapir rise rate and sedimentation rate lower and greater than 1, respectively. The radiocarbon ages obtained from several raised late Holocene strath terraces carved in the salt indicate uplift rates within the range of 36.5–12.1 mm/yr, consistent with geodetic data. The spatial variability of the uplift rates can be related to increasing flow rates towards the axis of the salt wall and potential along-strike variations. The relatively high diapir rise rates observed at Cardona diapir, unaffected by contractional displacement loading (tectonic squeezing), is attributed to the youthful stage of the salt extrusion and the low dynamic viscosity of the Cardona Saline Formation, with a low proportion of impurities and a significant amount of potash saltsAquest treball ha estat desenvolupat pel Projecte DIAPERNO ( PID2021-123189NB-I00) finançat pel Govern espanyol (Ministerio de Ciencia e Innovación)Elsevier2024info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionpeer-reviewedapplication/pdfhttp://hdl.handle.net/10256/25395http://hdl.handle.net/10256/25395Quaternary Science Reviews, 2024, vol. 324, art. núm. 108462Articles publicats (D-CCAA)reponame:Recercat. Dipósit de la Recerca de Catalunyainstname:Varias* (Consorci de Biblioteques Universitáries de Catalunya, Centre de Serveis Científics i Acadèmics de Catalunya)Inglésinfo:eu-repo/semantics/altIdentifier/doi/10.1016/j.quascirev.2023.108462info:eu-repo/semantics/altIdentifier/issn/0277-3791info:eu-repo/semantics/altIdentifier/eissn/1873-457XAttribution-NonCommercial 4.0 Internationalhttp://creativecommons.org/licenses/by-nc/4.0/info:eu-repo/semantics/openAccessoai:recercat.cat:10256/253952026-05-29T05:05:01Z
dc.title.none.fl_str_mv Late Quaternary morpho-stratigraphic record of diapir rise in the Cardona salt extrusion, NE Spain. Halokinetic sequences, raised terraces and uplift rates
title Late Quaternary morpho-stratigraphic record of diapir rise in the Cardona salt extrusion, NE Spain. Halokinetic sequences, raised terraces and uplift rates
spellingShingle Late Quaternary morpho-stratigraphic record of diapir rise in the Cardona salt extrusion, NE Spain. Halokinetic sequences, raised terraces and uplift rates
Pérez Villar, Guillermo
Diapirs -- Catalunya -- Cardona
Diapirs -- Catalonia -- Cardona
Estratigrafia -- Quaternari
Geology, Stratigraphic -- Quaternary
Salines (Geologia) -- Catalunya -- Cardona
Salt pans (Geology) -- Catalonia -- Cardona
Jaciments salins -- Catalunya -- Cardona
Salt deposits -- Catalonia -- Cardona
Radiocarboni, Mètode del
Radiocarbon dating
title_short Late Quaternary morpho-stratigraphic record of diapir rise in the Cardona salt extrusion, NE Spain. Halokinetic sequences, raised terraces and uplift rates
title_full Late Quaternary morpho-stratigraphic record of diapir rise in the Cardona salt extrusion, NE Spain. Halokinetic sequences, raised terraces and uplift rates
title_fullStr Late Quaternary morpho-stratigraphic record of diapir rise in the Cardona salt extrusion, NE Spain. Halokinetic sequences, raised terraces and uplift rates
title_full_unstemmed Late Quaternary morpho-stratigraphic record of diapir rise in the Cardona salt extrusion, NE Spain. Halokinetic sequences, raised terraces and uplift rates
title_sort Late Quaternary morpho-stratigraphic record of diapir rise in the Cardona salt extrusion, NE Spain. Halokinetic sequences, raised terraces and uplift rates
dc.creator.none.fl_str_mv Pérez Villar, Guillermo
Gutiérrez Santolalla, Francisco
Zarroca, Mario
Roqué i Pau, Carles
Benito-Calvo, Alfonso
Menció i Domingo, Anna
author Pérez Villar, Guillermo
author_facet Pérez Villar, Guillermo
Gutiérrez Santolalla, Francisco
Zarroca, Mario
Roqué i Pau, Carles
Benito-Calvo, Alfonso
Menció i Domingo, Anna
author_role author
author2 Gutiérrez Santolalla, Francisco
Zarroca, Mario
Roqué i Pau, Carles
Benito-Calvo, Alfonso
Menció i Domingo, Anna
author2_role author
author
author
author
author
dc.subject.none.fl_str_mv Diapirs -- Catalunya -- Cardona
Diapirs -- Catalonia -- Cardona
Estratigrafia -- Quaternari
Geology, Stratigraphic -- Quaternary
Salines (Geologia) -- Catalunya -- Cardona
Salt pans (Geology) -- Catalonia -- Cardona
Jaciments salins -- Catalunya -- Cardona
Salt deposits -- Catalonia -- Cardona
Radiocarboni, Mètode del
Radiocarbon dating
topic Diapirs -- Catalunya -- Cardona
Diapirs -- Catalonia -- Cardona
Estratigrafia -- Quaternari
Geology, Stratigraphic -- Quaternary
Salines (Geologia) -- Catalunya -- Cardona
Salt pans (Geology) -- Catalonia -- Cardona
Jaciments salins -- Catalunya -- Cardona
Salt deposits -- Catalonia -- Cardona
Radiocarboni, Mètode del
Radiocarbon dating
description Active diapirism has received very limited attention from the geomorphological and Quaternary Science perspective, despite the role played by this ground deformation process in the development of landforms and sedimentary environments, and the important practical implications associated with mobile salt structures (e,g., mining, hydrocarbon production, geostorage). The Cardona salt extrusion (NE Spain) was initiated in late Quaternary times from the post-shortening unroofing of the crest of a salt anticline by the entrenchment of the transverse Cardener River. Detailed mapping, outcrop analysis, geophysical data and trenching indicate that the diapir-flanking deposits show halokinetic complexes comprising two types of morpho-stratigraphic units: (1) an older flap of coarse-grained drapefolded colluvial deposits; and (2) younger lacustrine and fluvial deposits in peripheral depressions confined between the upturned colluvial flaps and the country rock slope. These synkinematic units record an overall relief inversion and correspond to the so-called wedge and hook halokinetic sequences, recording ratios between diapir rise rate and sedimentation rate lower and greater than 1, respectively. The radiocarbon ages obtained from several raised late Holocene strath terraces carved in the salt indicate uplift rates within the range of 36.5–12.1 mm/yr, consistent with geodetic data. The spatial variability of the uplift rates can be related to increasing flow rates towards the axis of the salt wall and potential along-strike variations. The relatively high diapir rise rates observed at Cardona diapir, unaffected by contractional displacement loading (tectonic squeezing), is attributed to the youthful stage of the salt extrusion and the low dynamic viscosity of the Cardona Saline Formation, with a low proportion of impurities and a significant amount of potash salts
publishDate 2024
dc.date.none.fl_str_mv 2024
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
peer-reviewed
format article
status_str publishedVersion
dc.identifier.none.fl_str_mv http://hdl.handle.net/10256/25395
http://hdl.handle.net/10256/25395
url http://hdl.handle.net/10256/25395
dc.language.none.fl_str_mv Inglés
language_invalid_str_mv Inglés
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/doi/10.1016/j.quascirev.2023.108462
info:eu-repo/semantics/altIdentifier/issn/0277-3791
info:eu-repo/semantics/altIdentifier/eissn/1873-457X
dc.rights.none.fl_str_mv Attribution-NonCommercial 4.0 International
http://creativecommons.org/licenses/by-nc/4.0/
info:eu-repo/semantics/openAccess
rights_invalid_str_mv Attribution-NonCommercial 4.0 International
http://creativecommons.org/licenses/by-nc/4.0/
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv application/pdf
dc.publisher.none.fl_str_mv Elsevier
publisher.none.fl_str_mv Elsevier
dc.source.none.fl_str_mv Quaternary Science Reviews, 2024, vol. 324, art. núm. 108462
Articles publicats (D-CCAA)
reponame:Recercat. Dipósit de la Recerca de Catalunya
instname:Varias* (Consorci de Biblioteques Universitáries de Catalunya, Centre de Serveis Científics i Acadèmics de Catalunya)
instname_str Varias* (Consorci de Biblioteques Universitáries de Catalunya, Centre de Serveis Científics i Acadèmics de Catalunya)
reponame_str Recercat. Dipósit de la Recerca de Catalunya
collection Recercat. Dipósit de la Recerca de Catalunya
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