<?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>2026-06-08T08:28:29Z</responseDate><request verb="GetRecord" identifier="oai:docta.ucm.es:20.500.14352/65234" metadataPrefix="qdc">https://docta.ucm.es/rest/oai/request</request><GetRecord><record><header><identifier>oai:docta.ucm.es:20.500.14352/65234</identifier><datestamp>2024-07-23T17:14:56Z</datestamp><setSpec>com_20.500.14352_14</setSpec><setSpec>col_20.500.14352_15</setSpec></header><metadata><qdc:qualifieddc xmlns:qdc="http://dspace.org/qualifieddc/" xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:dcterms="http://purl.org/dc/terms/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns:doc="http://www.lyncode.com/xoai" xsi:schemaLocation="http://purl.org/dc/elements/1.1/ http://dublincore.org/schemas/xmls/qdc/2006/01/06/dc.xsd http://purl.org/dc/terms/ http://dublincore.org/schemas/xmls/qdc/2006/01/06/dcterms.xsd http://dspace.org/qualifieddc/ http://www.ukoln.ac.uk/metadata/dcmi/xmlschema/qualifieddc.xsd">
   <dc:title>El Trías de Alcázar de San Juan (Región de La Mancha).</dc:title>
   <dc:creator>Yébenes, A.</dc:creator>
   <dc:creator>Marfil Pérez, Rafaela</dc:creator>
   <dc:creator>Soriano, J.</dc:creator>
   <dc:creator>Peña, José Andrés de la</dc:creator>
   <dc:creator>Díaz Molina, Margarita</dc:creator>
   <dcterms:abstract>Se ha levantado una columna litoestratigráfica de detalle entre Alcázar de San Juan y Campo dc Criptana, distinguiéndose seis unidades que en conjunto pasan de tener neto carácter detrítico en la base a facies evaporíticas en el techo. La potencia total es de 140 a 180 metros. Se definen los caracteres petrológicos y sedimentológicos, comparándose sus facies con los materiales triásicos de la Cordillera Ibérica y de la zona prebética.</dcterms:abstract>
   <dcterms:abstract>Six units have been differentiated in a detailed litho-stratigraphic column
between Alcázar de San Juan and Campo de Criptana. These six units present
a clear detrital character at the base which changes lo evaporitic facies
toward Ihe top.
The petrological and sedimentological characteristics are defined, comparing
their facies with Ihe Triassic materials of the Iberian Range and Ihe
prebetie zone.</dcterms:abstract>
   <dcterms:dateAccepted>2023-06-21T02:16:47Z</dcterms:dateAccepted>
   <dcterms:available>2023-06-21T02:16:47Z</dcterms:available>
   <dcterms:created>2023-06-21T02:16:47Z</dcterms:created>
   <dcterms:issued>1977</dcterms:issued>
   <dc:type>journal article</dc:type>
   <dc:identifier>https://hdl.handle.net/20.500.14352/65234</dc:identifier>
   <dc:identifier>0378-102X</dc:identifier>
   <dc:language>spa</dc:language>
   <dc:rights>open access</dc:rights>
   <dc:publisher>Servicio de Publicaciones de la Universidad Complutense de Madrid</dc:publisher>
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