<?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>2026-04-13T06:46:24Z</responseDate><request verb="GetRecord" identifier="oai:www.recercat.cat:2445/193583" metadataPrefix="qdc">https://recercat.cat/oai/request</request><GetRecord><record><header><identifier>oai:recercat.cat:2445/193583</identifier><datestamp>2025-12-05T14:31:34Z</datestamp><setSpec>com_2072_1057</setSpec><setSpec>col_2072_478917</setSpec><setSpec>col_2072_478923</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>Cannibalization of previous Na-rich clinopyroxenes by ascending basic magmas of the Garrotxa Volcanic Field (NE Spain)</dc:title>
   <dc:creator>Aulinas Juncà, Meritxell</dc:creator>
   <dc:creator>Gisbert Pinto, Guillem</dc:creator>
   <dc:creator>Gimeno Torrente, Domingo</dc:creator>
   <dc:creator>Gasperini, D.</dc:creator>
   <dc:subject>Geoquímica</dc:subject>
   <dc:subject>Magmatisme</dc:subject>
   <dc:subject>Garrotxa (Catalunya)</dc:subject>
   <dc:subject>Geochemistry</dc:subject>
   <dc:subject>Magmatism</dc:subject>
   <dc:subject>Garrotxa (Catalonia)</dc:subject>
   <dcterms:abstract>The Garrotxa Volcanic Field (GVF) is a Quaternary monogenetic volcanic field belonging to the NE Spain volcanic province, recording a Neogene alkaline intraplate magmatic activity consequence of the rift-type extensional tectonics that has affected the eastern margin of Iberia since late Oligocene.</dcterms:abstract>
   <dcterms:issued>2023-02-14T10:13:09Z</dcterms:issued>
   <dcterms:issued>2023-02-14T10:13:09Z</dcterms:issued>
   <dcterms:issued>2013-07-01</dcterms:issued>
   <dcterms:issued>2023-02-14T10:13:09Z</dcterms:issued>
   <dc:type>info:eu-repo/semantics/article</dc:type>
   <dc:type>info:eu-repo/semantics/publishedVersion</dc:type>
   <dc:relation>Reproducció del document publicat a: https://doi.org/10.1180/minmag.2013.077.5.1</dc:relation>
   <dc:relation>Mineralogical Magazine, 2013, vol. 77, num. 5, p. 631-631</dc:relation>
   <dc:relation>https://doi.org/10.1180/minmag.2013.077.5.1</dc:relation>
   <dc:rights>(c) Mineralogical Society, 2013</dc:rights>
   <dc:rights>info:eu-repo/semantics/openAccess</dc:rights>
   <dc:publisher>Mineralogical Society</dc:publisher>
   <dc:source>Articles publicats en revistes (Mineralogia, Petrologia i Geologia Aplicada)</dc:source>
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