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Título

The Campo de Dalias GNSS Network Unveils the Interaction between Roll-Back and Indentation Tectonics in the Gibraltar Arc

AutorGalindo-Zaldívar, Jesús; Gil, Antonio J.; Tendero-Salmerón, Víctor; Borque Arancón, María Jesús; Ercilla, Gemma CSIC ORCID ; González Castillo, Lourdes; Sánchez-Alzola, Alberto; Lacy Pérez de los Cobos, M.ª Clara de; Estrada, Ferran CSIC ORCID CVN ; Avilés, Manuel; Alfaro, Pedro; Madarieta-Txurruka, Asier; Chacón, Fernando
Palabras claveGNSS network
Active fold and fault interaction
Roll-back
Indentation tectonics
Gibraltar Arc
Fecha de publicaciónmar-2022
EditorMultidisciplinary Digital Publishing Institute
CitaciónSensors 22(6): 2128 (2022)
ResumenThe Gibraltar Arc includes the Betic and Rif Cordilleras surrounding the Alboran Sea; it is formed at the northwest–southeast Eurasia–Nubia convergent plate boundary in the westernmost Mediterranean. Since 2006, the Campo de Dalias GNSS network has monitored active tectonic deformation of the most seismically active area on the north coast of the Alboran Sea. Our results show that the residual deformation rates with respect to Eurasia range from 1.7 to 3.0 mm/year; roughly homogenous west-southwestward displacements of the northern sites occur, while the southern sites evidence irregular displacements towards the west and northwest. This deformation pattern supports simultaneous east-northeast–west-southwest extension, accommodated by normal and oblique faults, and north-northwest–south-southeast shortening that develops east-northeast–west-southwest folds. Moreover, the GNSS results point to dextral creep of the main northwest–southeast Balanegra Fault. These GNNS results thus reveal, for the first time, present-day interaction of the roll-back tectonics of the Rif–Gibraltar–Betic slab in the western part of the Gibraltar Arc with the indentation tectonics affecting the eastern and southern areas, providing new insights for improving tectonic models of arcuate orogens
Descripción12 pages, 7 figures, 1 table.-- Data Availability Statement: The data are included in Table 1 of this paper
Versión del editorhttps://doi.org/10.3390/s22062128
URIhttp://hdl.handle.net/10261/268085
DOI10.3390/s22062128
E-ISSN1424-8220
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