<?xml version="1.0" encoding="UTF-8"?><?xml-stylesheet type="text/xsl" href="static/style.xsl"?><OAI-PMH xmlns="http://www.openarchives.org/OAI/2.0/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/ http://www.openarchives.org/OAI/2.0/OAI-PMH.xsd"><responseDate>2026-06-01T02:08:53Z</responseDate><request verb="GetRecord" identifier="oai:docta.ucm.es:20.500.14352/128661" metadataPrefix="oai_dc">https://docta.ucm.es/rest/oai/request</request><GetRecord><record><header><identifier>oai:docta.ucm.es:20.500.14352/128661</identifier><datestamp>2025-12-10T00:56:32Z</datestamp><setSpec>com_20.500.14352_14</setSpec><setSpec>col_20.500.14352_15</setSpec></header><metadata><oai_dc:dc xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns:doc="http://www.lyncode.com/xoai" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
   <dc:title>Síntesis de la evolución geodinámica durante el Cuaternario de la zona oriental de la cuenca de Huércal-Overa (Almería, Cordilleras Béticas)</dc:title>
   <dc:creator>García Meléndez, Eduardo</dc:creator>
   <dc:creator>Goy Goy, José Luis</dc:creator>
   <dc:creator>Zazo Cardeña, Caridad</dc:creator>
   <dc:subject>551.4:551.79(460.358)</dc:subject>
   <dc:subject>551.24"626/627"(460.358)</dc:subject>
   <dc:subject>alluvial fans</dc:subject>
   <dc:subject>Geomorphology</dc:subject>
   <dc:subject>Neotectonics</dc:subject>
   <dc:subject>subsidence</dc:subject>
   <dc:subject>Quaternary</dc:subject>
   <dc:subject>Geodinámica</dc:subject>
   <dc:subject>2506.07 Geomorfología</dc:subject>
   <dc:subject>2507.07 Tectónica</dc:subject>
   <dc:description>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.</dc:description>
   <dc:description>Ministerio de Ciencia y Tecnología (España)</dc:description>
   <dc:description>Depto. de Geodinámica, Estratigrafía y Paleontología</dc:description>
   <dc:description>Fac. de Ciencias Geológicas</dc:description>
   <dc:description>TRUE</dc:description>
   <dc:description>pub</dc:description>
   <dc:date>2025-12-09T19:13:05Z</dc:date>
   <dc:date>2025-12-09T19:13:05Z</dc:date>
   <dc:date>2004</dc:date>
   <dc:type>journal article</dc:type>
   <dc:type>VoR</dc:type>
   <dc:identifier>https://hdl.handle.net/20.500.14352/128661</dc:identifier>
   <dc:identifier>1576-5172</dc:identifier>
   <dc:identifier>2792-2308</dc:identifier>
   <dc:language>spa</dc:language>
   <dc:relation>MCYT (BTE 2002-01691)</dc:relation>
   <dc:relation>MCYT (BTE 2002-01065)</dc:relation>
   <dc:relation>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.</dc:relation>
   <dc:rights>restricted access</dc:rights>
   <dc:format>application/pdf</dc:format>
   <dc:publisher>Sociedad Geológica de España</dc:publisher>
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