Lateral slip rate of Alhama de Murcia fault (SE Iberiam Peninsula) based on a morphotectonic analysis: comparison with paleoseismological data

To define the seismic potential of the left-lateral strike-slip Alhama de Murcia fault (SE Iberian Peninsula), we calculated its slip rate by measuring offset linear features of known age using a morphotectonic analysis. The Lorca-Totana section of the fault yielded a minimum slip rate of 1.0 ± 0.2...

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Autores: Ferrater Gómez, Marta, Ortuño Candela, Maria, Masana, Eulàlia, Martínez-Díaz, José J., Pallàs i Serra, Raimon, Perea Manera, Héctor, Baize, Stéphane, García Meléndez, Eduardo, Echeverria, Anna, Rockwell, Thomas K., Sharp, Warren D., Arrowsmith, Ramon
Formato: artículo
Estado:Versión aceptada para publicación
Fecha de publicación:2017
País:España
Recursos:Universidad de Barcelona
Repositorio:Dipòsit Digital de la UB
OAI Identifier:oai:diposit.ub.edu:2445/163722
Acesso em linha:https://hdl.handle.net/2445/163722
Access Level:acceso abierto
Palavra-chave:Paleosismologia
Tectònica
Múrcia (Múrcia)
Paleoseismology
Tectonics
Murcia (Murcia)
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spelling Lateral slip rate of Alhama de Murcia fault (SE Iberiam Peninsula) based on a morphotectonic analysis: comparison with paleoseismological dataFerrater Gómez, MartaOrtuño Candela, MariaMasana, EulàliaMartínez-Díaz, José J.Pallàs i Serra, RaimonPerea Manera, HéctorBaize, StéphaneGarcía Meléndez, EduardoEcheverria, AnnaRockwell, Thomas K.Sharp, Warren D.Arrowsmith, RamonPaleosismologiaTectònicaMúrcia (Múrcia)PaleoseismologyTectonicsMurcia (Murcia)To define the seismic potential of the left-lateral strike-slip Alhama de Murcia fault (SE Iberian Peninsula), we calculated its slip rate by measuring offset linear features of known age using a morphotectonic analysis. The Lorca-Totana section of the fault yielded a minimum slip rate of 1.0 ± 0.2 mm/a for the past 30 ka, based on a channel whose age is estimated by OSL technique. The minimum left-lateral slip rate of the Goñar-Lorca section is 1.6-1.7 mm/a for the past 200 ka, based on eight offset surface channels, previously mapped alluvial fans dated by TL, and by new U-series dating of pedogenic carbonate. The U-series technique was used here for first time in the Iberian Peninsula to date small amounts (mg) of pedogenic carbonate. According to the newly estimated slip rate values, the Alhama de Murcia fault is one of the most active faults in the Eastern Betics Shear Zone. These values are larger and have fewer uncertainties in comparison with previous slip rates estimations. In the Lorca-Totana section, the new lateral slip rate is compared with a slip rate calculated by means of a paleoseismic study showing good agreement between the values obtained with the two approaches. We encourage the combination of paleoseismology and morphotectonic analysis to obtain reliable slip rates for faults with scarce evidence of late Holocene slip.Elsevier Ltd2017info:eu-repo/semantics/articleinfo:eu-repo/semantics/acceptedVersionapplication/pdfhttps://hdl.handle.net/2445/163722Articles 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.quaint.2017.02.018Quaternary International, 2017, vol. 451, p. 87-100https://doi.org/10.1016/j.quaint.2017.02.018cc-by-nc-nd (c) Elsevier Ltd, 2017http://creativecommons.org/licenses/by-nc-nd/3.0/esinfo:eu-repo/semantics/openAccessoai:diposit.ub.edu:2445/1637222026-05-27T06:46:51Z
dc.title.none.fl_str_mv Lateral slip rate of Alhama de Murcia fault (SE Iberiam Peninsula) based on a morphotectonic analysis: comparison with paleoseismological data
title Lateral slip rate of Alhama de Murcia fault (SE Iberiam Peninsula) based on a morphotectonic analysis: comparison with paleoseismological data
spellingShingle Lateral slip rate of Alhama de Murcia fault (SE Iberiam Peninsula) based on a morphotectonic analysis: comparison with paleoseismological data
Ferrater Gómez, Marta
Paleosismologia
Tectònica
Múrcia (Múrcia)
Paleoseismology
Tectonics
Murcia (Murcia)
title_short Lateral slip rate of Alhama de Murcia fault (SE Iberiam Peninsula) based on a morphotectonic analysis: comparison with paleoseismological data
title_full Lateral slip rate of Alhama de Murcia fault (SE Iberiam Peninsula) based on a morphotectonic analysis: comparison with paleoseismological data
title_fullStr Lateral slip rate of Alhama de Murcia fault (SE Iberiam Peninsula) based on a morphotectonic analysis: comparison with paleoseismological data
title_full_unstemmed Lateral slip rate of Alhama de Murcia fault (SE Iberiam Peninsula) based on a morphotectonic analysis: comparison with paleoseismological data
title_sort Lateral slip rate of Alhama de Murcia fault (SE Iberiam Peninsula) based on a morphotectonic analysis: comparison with paleoseismological data
dc.creator.none.fl_str_mv Ferrater Gómez, Marta
Ortuño Candela, Maria
Masana, Eulàlia
Martínez-Díaz, José J.
Pallàs i Serra, Raimon
Perea Manera, Héctor
Baize, Stéphane
García Meléndez, Eduardo
Echeverria, Anna
Rockwell, Thomas K.
Sharp, Warren D.
Arrowsmith, Ramon
author Ferrater Gómez, Marta
author_facet Ferrater Gómez, Marta
Ortuño Candela, Maria
Masana, Eulàlia
Martínez-Díaz, José J.
Pallàs i Serra, Raimon
Perea Manera, Héctor
Baize, Stéphane
García Meléndez, Eduardo
Echeverria, Anna
Rockwell, Thomas K.
Sharp, Warren D.
Arrowsmith, Ramon
author_role author
author2 Ortuño Candela, Maria
Masana, Eulàlia
Martínez-Díaz, José J.
Pallàs i Serra, Raimon
Perea Manera, Héctor
Baize, Stéphane
García Meléndez, Eduardo
Echeverria, Anna
Rockwell, Thomas K.
Sharp, Warren D.
Arrowsmith, Ramon
author2_role author
author
author
author
author
author
author
author
author
author
author
dc.subject.none.fl_str_mv Paleosismologia
Tectònica
Múrcia (Múrcia)
Paleoseismology
Tectonics
Murcia (Murcia)
topic Paleosismologia
Tectònica
Múrcia (Múrcia)
Paleoseismology
Tectonics
Murcia (Murcia)
description To define the seismic potential of the left-lateral strike-slip Alhama de Murcia fault (SE Iberian Peninsula), we calculated its slip rate by measuring offset linear features of known age using a morphotectonic analysis. The Lorca-Totana section of the fault yielded a minimum slip rate of 1.0 ± 0.2 mm/a for the past 30 ka, based on a channel whose age is estimated by OSL technique. The minimum left-lateral slip rate of the Goñar-Lorca section is 1.6-1.7 mm/a for the past 200 ka, based on eight offset surface channels, previously mapped alluvial fans dated by TL, and by new U-series dating of pedogenic carbonate. The U-series technique was used here for first time in the Iberian Peninsula to date small amounts (mg) of pedogenic carbonate. According to the newly estimated slip rate values, the Alhama de Murcia fault is one of the most active faults in the Eastern Betics Shear Zone. These values are larger and have fewer uncertainties in comparison with previous slip rates estimations. In the Lorca-Totana section, the new lateral slip rate is compared with a slip rate calculated by means of a paleoseismic study showing good agreement between the values obtained with the two approaches. We encourage the combination of paleoseismology and morphotectonic analysis to obtain reliable slip rates for faults with scarce evidence of late Holocene slip.
publishDate 2017
dc.date.none.fl_str_mv 2017
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/2445/163722
url https://hdl.handle.net/2445/163722
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.quaint.2017.02.018
Quaternary International, 2017, vol. 451, p. 87-100
https://doi.org/10.1016/j.quaint.2017.02.018
dc.rights.none.fl_str_mv cc-by-nc-nd (c) Elsevier Ltd, 2017
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 Ltd, 2017
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 Ltd
publisher.none.fl_str_mv Elsevier Ltd
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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score 15,301603