<?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>2026-06-29T07:27:25Z</responseDate><request verb="GetRecord" identifier="oai:docta.ucm.es:20.500.14352/65047" metadataPrefix="oai_dc">https://docta.ucm.es/rest/oai/request</request><GetRecord><record><header><identifier>oai:docta.ucm.es:20.500.14352/65047</identifier><datestamp>2024-07-29T14:34:30Z</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>El paisaje eólico de la llanura aluvial de San Juan (Llanura Manchega Central)</dc:title>
   <dc:creator>Pérez González, Alfredo José</dc:creator>
   <dc:creator>Aleixandre, T.</dc:creator>
   <dc:creator>Pinilla, A.</dc:creator>
   <dc:creator>Gallardo, J.</dc:creator>
   <dc:subject>551.311.13(460)</dc:subject>
   <dc:subject>(460)551.311.13</dc:subject>
   <dc:subject>Dunas</dc:subject>
   <dc:subject>España</dc:subject>
   <dc:subject>Sand dunes</dc:subject>
   <dc:subject>Spain</dc:subject>
   <dc:subject>Geodinámica</dc:subject>
   <dc:subject>2507 Geofísica</dc:subject>
   <dc:description>El campo dunar de la Llanura aluvial de San Juan, esta caracterizado por la presencia de dunas arcillosas, limosas o limo-arcillosas. Morfológicamente, son dunas de tipo parabólico y otras con aspecto "cónico", "transverso" o "longitudinal", construidas por paleovientos efectivos que provenían del W y SI-J.. Finalmente, se discute la edad y origen de estos complejos dunares.</dc:description>
   <dc:description>The dunes of the San Juan alluvial p1ain consists most characteristically of c1ayey, silty, and c1ayey si1ty
dunes, which morphologically are most common1y of parabolic type , but dome-shaped, transverse and linear dunes are present as well. These were built up by effective winds coming from the W and SW. Finally, both the age and genesis of these dunes is discussed.</dc:description>
   <dc:description>Depto. de Geodinámica, Estratigrafía y Paleontología</dc:description>
   <dc:description>Fac. de Ciencias Geológicas</dc:description>
   <dc:description>FALSE</dc:description>
   <dc:description>pub</dc:description>
   <dc:date>2023-06-21T02:10:48Z</dc:date>
   <dc:date>2023-06-21T02:10:48Z</dc:date>
   <dc:date>1983</dc:date>
   <dc:type>journal article</dc:type>
   <dc:identifier>https://hdl.handle.net/20.500.14352/65047</dc:identifier>
   <dc:identifier>0213-4497</dc:identifier>
   <dc:language>spa</dc:language>
   <dc:rights>open access</dc:rights>
   <dc:format>application/pdf</dc:format>
   <dc:publisher>Seminario de Estudos Galegos. Area de Xeoloxía e Minería ;  Instituto Universitario de Xeoloxía "Isidro Parga Pondal"</dc:publisher>
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