<?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>2026-04-18T07:58:21Z</responseDate><request verb="GetRecord" identifier="oai:www.recercat.cat:2445/42029" metadataPrefix="oai_dc">https://recercat.cat/oai/request</request><GetRecord><record><header><identifier>oai:recercat.cat:2445/42029</identifier><datestamp>2025-12-05T17:04:44Z</datestamp><setSpec>com_2072_1057</setSpec><setSpec>col_2072_478804</setSpec><setSpec>col_2072_478917</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>Resultados preliminares en la caracterización geométrica 3D de un litosoma arenoso de progradación deltaica mediante Georadar (GPR) (Fm. Arenisca de Roda, Eoceno, Cuenca de Graus-Tremp).</dc:title>
   <dc:creator>Coll, M.</dc:creator>
   <dc:creator>López Blanco, Miguel</dc:creator>
   <dc:creator>Marcuello Pascual, Alejandro</dc:creator>
   <dc:subject>Prospecció geofísica</dc:subject>
   <dc:subject>Geomagnetisme</dc:subject>
   <dc:subject>Eocè</dc:subject>
   <dc:subject>Geophysical exploration</dc:subject>
   <dc:subject>Geomagnetism</dc:subject>
   <dc:subject>Eocene Epoch</dc:subject>
   <dc:description>A set of GPR profiles have been recorded in order to determine the 3D geometry of a prograding delta-front sandbody (Roda sandstone formation, Eocene, Graus-Tremp basin). Common Mid Points (CMP) also have been recorded to obtain the velocity of the electromagnetic wave in ground. In order to build the topsurface of a 3D prism a set of topographic points have been acquired. Most of the GPR profiles are oriented parallel to the progradation direction (NNE-SSW) and show the expected geometries. The 3D prism has been built from the individual profiles, which shows the three dimensional geometry of the sandy lithosome.</dc:description>
   <dc:date>2013-05-03T15:29:55Z</dc:date>
   <dc:date>2013-05-03T15:29:55Z</dc:date>
   <dc:date>2007</dc:date>
   <dc:date>2013-05-03T15:29:55Z</dc:date>
   <dc:type>info:eu-repo/semantics/article</dc:type>
   <dc:type>info:eu-repo/semantics/publishedVersion</dc:type>
   <dc:identifier>0213-683X</dc:identifier>
   <dc:identifier>https://hdl.handle.net/2445/42029</dc:identifier>
   <dc:identifier>551465</dc:identifier>
   <dc:language>spa</dc:language>
   <dc:relation>Geogaceta, 2007, vol. 41, p. 51-54</dc:relation>
   <dc:rights>(c) Sociedad Geológica de España, 2007</dc:rights>
   <dc:rights>info:eu-repo/semantics/openAccess</dc:rights>
   <dc:format>4 p.</dc:format>
   <dc:format>application/pdf</dc:format>
   <dc:publisher>Sociedad Geológica de España</dc:publisher>
   <dc:source>Articles publicats en revistes (Dinàmica de la Terra i l'Oceà)</dc:source>
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