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Active Faults in Iberia

AuthorsSanz de Galdeano, Carlos ; Azañón, José Miguel ; Cabral, João; Ruano, P.; Alfaro, P.; Canora, Carolina; Ferrater, M.; García-Tortosa, Francisco Juan; García Mayordomo, Julián; Gràcia, Eulàlia ; Insua Arévalo, Miguel; Jiménez Bonilla, A.; Gilles Lacan, Pierre; Marín-Lechado, C.; Martín Banda, R.; Martín-González, Fidel; Martín-Rojas, Iván; Martínez-Díaz, J. J. ; Masana, E.; Ortuño, María; Pedrera, A.; Perea, Héctor ; Simón, José Luis
Issue Date2020
CitationThe Geology of Iberia: A Geodynamic Approach 5: 33-75 (2020)
The Geology of Iberia: A Geodynamic Approach : Active Processes: Seismicity, Active Faulting and Relief: 33-75 (2020)
The Geology of Iberia: A Geodynamic Approach : Active Processes: Seismicity, Active Faulting and Relief : Active Faults in Iberia 4(7): 33-75 (2020)
AbstractThe distribution of active faults in the Iberian Peninsula is not homogeneous, being mainly present, but not only, in areas affected by the Alpine Orogeny. They are located in several regions: (1) The Iberian Massif, including Portugal, and Galicia and Cantabrian Mountains in the North, (2) The Pyrenees, (3) The NE of Iberia, (4) The Iberian Cordillera, and (5) The Betic Cordillera. The Pyrenees, the Iberian Cordillera, and particularly the Betic Cordillera are the most active regions. These faults have being considered active in a broad sense, that is to say, corresponding to faults that, at least, present movements during the Quaternary, not restricting them only to those presenting displacements during the late 10,000 years. Although important, faults situated offshore have not being included in the present review
Description43 pages, 9 figures, 1 table
Publisher version (URL)https://doi.org/10.1007/978-3-030-10931-8_4
Identifiersisbn: 978-3-030-10930-1
isbn: 978-3-030-10931-8
issn: 2364-6438
e-issn: 2364-6446
Appears in Collections:(IACT) Artículos
(ICM) Libros y partes de libros
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