<?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>2026-08-22T19:56:51Z</responseDate><request verb="GetRecord" identifier="oai:docta.ucm.es:20.500.14352/138564" metadataPrefix="mods">https://docta.ucm.es/rest/oai/request</request><GetRecord><record><header><identifier>oai:docta.ucm.es:20.500.14352/138564</identifier><datestamp>2026-07-15T23:51:23Z</datestamp><setSpec>com_20.500.14352_14</setSpec><setSpec>col_20.500.14352_15</setSpec></header><metadata><mods:mods xmlns:mods="http://www.loc.gov/mods/v3" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns:doc="http://www.lyncode.com/xoai" xsi:schemaLocation="http://www.loc.gov/mods/v3 http://www.loc.gov/standards/mods/v3/mods-3-1.xsd">
   <mods:name>
      <mods:namePart>Calvet, F.</mods:namePart>
   </mods:name>
   <mods:name>
      <mods:namePart>López Gómez, José Trinidad</mods:namePart>
   </mods:name>
   <mods:name>
      <mods:namePart>Galindo Francisco, María Del Carmen</mods:namePart>
   </mods:name>
   <mods:name>
      <mods:namePart>Tucker, M.E.</mods:namePart>
   </mods:name>
   <mods:name>
      <mods:namePart>Arche, Alfredo</mods:namePart>
   </mods:name>
   <mods:extension>
      <mods:dateAvailable encoding="iso8601">2026-07-15T09:16:46Z</mods:dateAvailable>
   </mods:extension>
   <mods:extension>
      <mods:dateAccessioned encoding="iso8601">2026-07-15T09:16:46Z</mods:dateAccessioned>
   </mods:extension>
   <mods:originInfo>
      <mods:dateIssued encoding="iso8601">2001</mods:dateIssued>
   </mods:originInfo>
   <mods:identifier type="citation">Calvet, F. et al. (2001) «Dolomías de gran escala en las plataformas epeírícas triásicas del este de la Península Ibérica», Geotemas (Madrid), 3, pp. 105-108.</mods:identifier>
   <mods:identifier type="issn">1576-5172</mods:identifier>
   <mods:identifier type="uri">https://hdl.handle.net/20.500.14352/138564</mods:identifier>
   <mods:identifier type="essn">2792-2308</mods:identifier>
   <mods:identifier type="officialurl">https://sociedadgeologica.org/publicaciones/geotemas/geo-temas-3-2-vol/</mods:identifier>
   <mods:identifier type="relatedurl">https://sociedadgeologica.org/publicaciones/geotemas/</mods:identifier>
   <mods:abstract>The Triassic of the Iberian Peninsula presents three carbonate epeiric platforms (Lower Muschelkalk, Upper Muschelkalk and Imón Fm.). These three carbonate platforms are intensively dolomitized with a lower part made up of grey dolomites and an upper part of white dolomites. The white dolomites are sabkha-type dolomites and the grey dolomites reflux-type dolomites. The petrography stable isotopes and Sr isotopes of the grey and white dolomites suggest a late recrystallization process related to deep burial or hydrothermal conditions during the Jurassic-Cretaceous rifting.</mods:abstract>
   <mods:language>
      <mods:languageTerm>spa</mods:languageTerm>
   </mods:language>
   <mods:accessCondition type="useAndReproduction">open access</mods:accessCondition>
   <mods:titleInfo>
      <mods:title>Dolomías de gran escala en las plataformas epeírícas triásicas del este de la Península Ibérica</mods:title>
   </mods:titleInfo>
   <mods:genre>journal article</mods:genre>
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