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http://hdl.handle.net/10261/202011
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Título: | Extension in the Western Mediterranean |
Autor: | Galindo-Zaldívar, Jesús; Braga, J. C.; Marín-Lechado, Carlos CSIC ORCID; Ercilla, Gemma CSIC ORCID ; Martín, José M.; Pedrera Parias, Antonio CSIC ORCID; Casas, David CSIC ORCID ; Aguirre, Julio; Ruiz Constán, Ana CSIC ORCID; Estrada, Ferran CSIC ORCID CVN ; Puga-Bernabéu, Ángel; Sanz de Galdeano, Carlos CSIC ORCID; Juan, Carmen CSIC ORCID ; García-Alix, Antonio CSIC ORCID; Vázquez, Juan Tomás; Alonso, Belén CSIC ORCID | Fecha de publicación: | 2019 | Editor: | Springer Nature | Citación: | The Geology of Iberia: A Geodynamic Approach : Cenozoic Basins 3: 61-103 (2019) Regional Geology Reviews 3: 61-103 (2019) |
Resumen: | The Miocene is an essential period in the configuration of the present-day relief of the Betic Cordillera and the South Iberian continental margin, which determined the structure and evolution of the Neogene sedimentary basins (Fig. 3.1). The crustal thinning processes that occurred during the early and middle Miocene, after the main metamorphic events, generated major low-angle normal faults that separate the main metamorphic complexes. Although a wide variety of tectonic models have been proposed for this setting, most of them are related to delamination or to subduction with associated roll-back. During the late Miocene, the relatively flat and low relief of the continental crust facilitated the accumulation of sedimentary deposits, which are interlayered with volcanic rocks in the eastern Betic Cordillera and Alborán Sea. The continuous Eurasian-African convergence finally produced regional uplift since the late Miocene and the development of large late regional E-W to NE-SW folds, which determine the main reliefs | Descripción: | 43 pages, 31 figures | Versión del editor: | https://doi.org/10.1007/978-3-030-11190-8_3 | URI: | http://hdl.handle.net/10261/202011 | DOI: | 10.1007/978-3-030-11190-8_3 | ISSN: | 2364-6438 | E-ISSN: | 2364-6446 | Identificadores: | isbn: 978-3-030-11189-2 isbn: 978-3-030-11190-8 |
Aparece en las colecciones: | (IACT) Libros y partes de libros (ICM) Libros y partes de libros (IGME) Libros y partes de libros |
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