2026-06-28T20:24:25Zhttps://docta.ucm.es/rest/oai/request

oai:docta.ucm.es:20.500.14352/1286612025-12-10T00:56:32Zcom_20.500.14352_14col_20.500.14352_15

Síntesis de la evolución geodinámica durante el Cuaternario de la zona oriental de la cuenca de Huércal-Overa (Almería, Cordilleras Béticas) García Meléndez, Eduardo Goy Goy, José Luis Zazo Cardeña, Caridad The landscape of the eastern Huércal-Overa Basin reflects the influence of a tectonic context thataffected its younger landforms, and involved Quaternary neotectonic activity and the dominantalluvial sedimentary environment. From sedimentary descriptions, aerial photo-interpretation, geo-morphological mapping and the use of GIS techniques, the geodynamic evolution of this part ofthe Huércal-Overa basin during the late Pliocene and Quaternary has been reconstructed, emerging a complicated pattern. The main tectonic activity is associated with the entrance of the left-lateral strike-slip Lorca-Alhama fault (oriented NE-SW) in the Huércal-Overa basin. The interactionof this fault with earlier ENE-WSW to E-W faults inherited from the opening stage of the basinduring the Miocene formed a subsiding area (the Cubeta del Saltador) with pull-apart characteristics superimposed on the previous Miocene basin, and tectonic highs in both the northern and eastern margins. 2025-12-09T19:13:05Z 2025-12-09T19:13:05Z 2004 journal article García Meléndez, Eduardo, et al. «Síntesis de la evolución geodinámica durante el Cuaternario de la zona oriental de la cuenca de Huércal-Overa (Almería, Cordilleras Béticas)». Geotemas, n.º 6-4, 2004, pp. 227-30, https://sge.usal.es/archivos/GEO_TEMAS/Geo_temas_6_4sge.pdf. 1576-5172 https://hdl.handle.net/20.500.14352/128661 2792-2308 https://sge.usal.es/archivos/GEO_TEMAS/Geo_temas_6_4sge.pdf spa MCYT (BTE 2002-01691) MCYT (BTE 2002-01065) restricted access Sociedad Geológica de España