Miocene tectono-sedimentary evolution of the eastern external Betic Cordillera (Spain)
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Título: | Miocene tectono-sedimentary evolution of the eastern external Betic Cordillera (Spain) |
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Autor/es: | Martín-Martín, Manuel | Guerrera, Francesco | Rodríguez-Estrella, Tomás | Serrano Lozano, Francisco | Alcalá, Francisco J. | Raffaelli, Giuliana | Tramontana, Mario |
Grupo/s de investigación o GITE: | Evolución Geodinámica de la Cordillera Bética Oriental y de la Plataforma Marina de Alicante |
Centro, Departamento o Servicio: | Universidad de Alicante. Departamento de Ciencias de la Tierra y del Medio Ambiente |
Palabras clave: | Western mediterranean | Foredeep record | Sedimentary supply | Depositional sequences | Tectono-sedimentary evolutionary model |
Área/s de conocimiento: | Geodinámica Interna |
Fecha de publicación: | 13-jul-2018 |
Editor: | Taylor & Francis |
Cita bibliográfica: | Geodinamica Acta. 2018, 30(1): 265-286. doi:10.1080/09853111.2018.1493879 |
Resumen: | An interdisciplinary study of Miocene successions in the eastern External Betic Zone (South Iberian Margin) was carried out. Evidences of syn-sedimentary tectonic activity were recognized. The results enabled a better reconstruction of the stratigraphic architecture (with an improved chronostratigraphic resolution) in the framework of the Miocene foredeep evolution of the eastern EBZ. Two main depositional sequences were dated as uppermost Burdigalian-upper Serravallian p.p. and middle-upper Tortonian. p.p., respectively. The vertical and lateral diversification of lithofacies associations and thicknesses resulted from the syn-depositional tectonic complexity of the area. A great variety of sedimentary depositional realms is due to different subsidence rates, and the growing of anticlines and synclines during the Langhian p.p.-Serravallian. After a regression with an early Tortonian erosional gap, platform to hemipelagic realms developed during the middle Tortonian. The end of the sedimentation coincided with the emplacement of an important olisthostrome-like mass consisting of Triassic material related to either the development of thrust systems or diapirs emerged in the middle-late Tortonian, during the nappe emplacement. Correlations with other external sectors of the Betic Chain, and the external domains of the Rif, Tell, and northern Apennine Chains highlighted a similar Miocene foredeep evolution during the building of these orogens. |
Patrocinador/es: | CGL2016-75679-P; Research supported by Grants from Urbino University (Responsible M. Tramontana) |
URI: | http://hdl.handle.net/10045/77576 |
ISSN: | 0985-3111 (Print) | 1778-3593 (Online) |
DOI: | 10.1080/09853111.2018.1493879 |
Idioma: | eng |
Tipo: | info:eu-repo/semantics/article |
Derechos: | © 2018 The Author(s). Published by Informa UK Limited, trading as Taylor & Francis Group. This is an Open Access article distributed under the terms of the Creative Commons Attribution License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. |
Revisión científica: | si |
Versión del editor: | https://doi.org/10.1080/09853111.2018.1493879 |
Aparece en las colecciones: | INV - GEODIN - Artículos de Revistas |
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