García Meléndez, EduardoGoy Goy, José LuisZazo Cardeña, Caridad2025-12-092025-12-092004García 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.1576-5172https://hdl.handle.net/20.500.14352/128661The 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.spajournal article2792-2308https://sge.usal.es/archivos/GEO_TEMAS/Geo_temas_6_4sge.pdfrestricted access551.4:551.79(460.358)551.24"626/627"(460.358)alluvial fansGeomorphologyNeotectonicssubsidenceQuaternaryGeodinámica2506.07 Geomorfología2507.07 Tectónica