<?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>2026-07-06T11:34:38Z</responseDate><request verb="GetRecord" identifier="oai:docta.ucm.es:20.500.14352/49428" metadataPrefix="mods">https://docta.ucm.es/rest/oai/request</request><GetRecord><record><header><identifier>oai:docta.ucm.es:20.500.14352/49428</identifier><datestamp>2024-07-19T16:40:43Z</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>Dahlquist, Juan A.</mods:namePart>
   </mods:name>
   <mods:name>
      <mods:namePart>Alasino, Pablo H.</mods:namePart>
   </mods:name>
   <mods:name>
      <mods:namePart>Galindo Francisco, María Del Carmen</mods:namePart>
   </mods:name>
   <mods:extension>
      <mods:dateAvailable encoding="iso8601">2023-06-20T09:25:09Z</mods:dateAvailable>
   </mods:extension>
   <mods:extension>
      <mods:dateAccessioned encoding="iso8601">2023-06-20T09:25:09Z</mods:dateAccessioned>
   </mods:extension>
   <mods:originInfo>
      <mods:dateIssued encoding="iso8601">2005</mods:dateIssued>
   </mods:originInfo>
   <mods:identifier type="issn">0213-683X</mods:identifier>
   <mods:identifier type="uri">https://hdl.handle.net/20.500.14352/49428</mods:identifier>
   <mods:identifier type="officialurl">http://www.sociedadgeologica.es/publicaciones_geogaceta.html</mods:identifier>
   <mods:abstract>Comparative compositional studies between two peraluminous unit with magmatic andalucite and cordierite
indicate that they were produced by partial melting of two differents metasedimentary source rocks. We
conclude that geochemical studies from peraluminous unit contributes to define the source rocks and to
constrain the pre-orogenic geotectonic environment</mods:abstract>
   <mods:language>
      <mods:languageTerm>spa</mods:languageTerm>
   </mods:language>
   <mods:accessCondition type="useAndReproduction">open access</mods:accessCondition>
   <mods:titleInfo>
      <mods:title>Granitoides peraluminosos y su relación con las rocas fuentes</mods:title>
   </mods:titleInfo>
   <mods:genre>journal article</mods:genre>
</mods:mods></metadata></record></GetRecord></OAI-PMH>