Gravimetric survey and modelling of a tectonic indenter boundary: The Palomares Fault Zone (Betic Cordillera, Iberia)
, pages, 7 figures.-- Data availability: Data will be made available on request
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Format: | artículo biblioteca |
Language: | English |
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Elsevier
2024
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Subjects: | Tectonic indentation, Strike-slip faults, Palomares Fault Zone, Gravity models, Eastern Betic Shear Zone, |
Online Access: | http://hdl.handle.net/10261/341693 http://dx.doi.org/10.13039/501100011011 http://dx.doi.org/10.13039/501100003329 http://dx.doi.org/10.13039/501100004837 http://dx.doi.org/10.13039/501100011033 |
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dig-icm-es-10261-3416932024-01-06T05:30:20Z Gravimetric survey and modelling of a tectonic indenter boundary: The Palomares Fault Zone (Betic Cordillera, Iberia) Tendero-Salmerón, Víctor Ercilla, Gemma González Castillo, Lourdes Madarieta-Txurruka, Asier Martínez-Moreno, Francisco José Estrada, Ferran Galindo-Zaldívar, Jesús Ministerio de Economía y Competitividad (España) Ministerio de Ciencia e Innovación (España) Junta de Andalucía Agencia Estatal de Investigación (España) Tectonic indentation Strike-slip faults Palomares Fault Zone Gravity models Eastern Betic Shear Zone , pages, 7 figures.-- Data availability: Data will be made available on request New gravimetric data are improving our understanding of the Palomares Fault Zone (PFZ) that accommodates the Águilas Arc tectonic indentation (eastern Betic Cordillera, SE Iberia) in the context of the Eurasia-Africa convergence. The PFZ limits the sedimentary infill geometry of the Vera and Pulpí Basins, and the western Guadalentín Corridor, which are located along the western boundary of the arc. Gravity anomaly models are in agreement with previous tectonic interpretations that suggest that the PFZ fragments and bends the depocenters of those basins, as it has been proposed for the antiforms (ranges) that are located eastwards. Furthermore, the gravity anomaly models show that the PFZ extends from the Cabrera Range to the Almagrera Range and ends in the north at the Pulpí Basin, where the basin infill is only deformed by a gentle symmetrical synform. As a consequence, the PFZ is (i) confined to the southern zone, where the deformation is most intense due to the displacement of the tectonic indenter, and (ii) disconnected from the front of the Águilas Arc and the Alhama de Murcia Fault (part of the Eastern Betic Shear Zone, EBSZ). The new extend of the PFZ we have documented supposes the structural segmentation of the EBSZ and reduces both seismotectonic and structural significances of the PFZ. The study of the PFZ shows that the boundaries of the indenter are the locus for diffused deformation accommodated by local-scale faulting along with structural rotations and deflections, rather than localized strike-slip faulting along the whole indenter margin This study was supported by projects CGL2016-80687-R AEI/FEDER, PID2022-136678NB-I00, AEI /FEDER, P18-RT-3275, B-RNM-301-UGR18 and RNM148 (Junta de Andalucía/FEDER). V.T.S. was supported by the FPU PhD grant (16/04038). ICM-CSIC author acknowledges the Severo Ochoa funding from the Spanish government through the “Severo Ochoa Centre of Excellence” accreditation (CEX2019-000928-S) Peer reviewed 2024-01-05T07:48:49Z 2024-01-05T07:48:49Z 2024 artículo http://purl.org/coar/resource_type/c_6501 Tectonophysics: 230147 (2024) 0040-1951 CEX2019-000928-S http://hdl.handle.net/10261/341693 10.1016/j.tecto.2023.230147 1879-3266 http://dx.doi.org/10.13039/501100011011 http://dx.doi.org/10.13039/501100003329 http://dx.doi.org/10.13039/501100004837 http://dx.doi.org/10.13039/501100011033 en #PLACEHOLDER_PARENT_METADATA_VALUE# #PLACEHOLDER_PARENT_METADATA_VALUE# info:eu-repo/grantAgreement/MINECO//CGL2016-80687-R info:eu-repo/grantAgreement/MICIN//PID2022-136678NB-I00 Postprint https://doi.org/10.1016/j.tecto.2023.230147 Sí open Elsevier |
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Tectonic indentation Strike-slip faults Palomares Fault Zone Gravity models Eastern Betic Shear Zone Tectonic indentation Strike-slip faults Palomares Fault Zone Gravity models Eastern Betic Shear Zone |
spellingShingle |
Tectonic indentation Strike-slip faults Palomares Fault Zone Gravity models Eastern Betic Shear Zone Tectonic indentation Strike-slip faults Palomares Fault Zone Gravity models Eastern Betic Shear Zone Tendero-Salmerón, Víctor Ercilla, Gemma González Castillo, Lourdes Madarieta-Txurruka, Asier Martínez-Moreno, Francisco José Estrada, Ferran Galindo-Zaldívar, Jesús Gravimetric survey and modelling of a tectonic indenter boundary: The Palomares Fault Zone (Betic Cordillera, Iberia) |
description |
, pages, 7 figures.-- Data availability: Data will be made available on request |
author2 |
Ministerio de Economía y Competitividad (España) |
author_facet |
Ministerio de Economía y Competitividad (España) Tendero-Salmerón, Víctor Ercilla, Gemma González Castillo, Lourdes Madarieta-Txurruka, Asier Martínez-Moreno, Francisco José Estrada, Ferran Galindo-Zaldívar, Jesús |
format |
artículo |
topic_facet |
Tectonic indentation Strike-slip faults Palomares Fault Zone Gravity models Eastern Betic Shear Zone |
author |
Tendero-Salmerón, Víctor Ercilla, Gemma González Castillo, Lourdes Madarieta-Txurruka, Asier Martínez-Moreno, Francisco José Estrada, Ferran Galindo-Zaldívar, Jesús |
author_sort |
Tendero-Salmerón, Víctor |
title |
Gravimetric survey and modelling of a tectonic indenter boundary: The Palomares Fault Zone (Betic Cordillera, Iberia) |
title_short |
Gravimetric survey and modelling of a tectonic indenter boundary: The Palomares Fault Zone (Betic Cordillera, Iberia) |
title_full |
Gravimetric survey and modelling of a tectonic indenter boundary: The Palomares Fault Zone (Betic Cordillera, Iberia) |
title_fullStr |
Gravimetric survey and modelling of a tectonic indenter boundary: The Palomares Fault Zone (Betic Cordillera, Iberia) |
title_full_unstemmed |
Gravimetric survey and modelling of a tectonic indenter boundary: The Palomares Fault Zone (Betic Cordillera, Iberia) |
title_sort |
gravimetric survey and modelling of a tectonic indenter boundary: the palomares fault zone (betic cordillera, iberia) |
publisher |
Elsevier |
publishDate |
2024 |
url |
http://hdl.handle.net/10261/341693 http://dx.doi.org/10.13039/501100011011 http://dx.doi.org/10.13039/501100003329 http://dx.doi.org/10.13039/501100004837 http://dx.doi.org/10.13039/501100011033 |
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