<?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>2026-06-29T07:43:52Z</responseDate><request verb="GetRecord" identifier="oai:docta.ucm.es:20.500.14352/121476" metadataPrefix="oai_dc">https://docta.ucm.es/rest/oai/request</request><GetRecord><record><header><identifier>oai:docta.ucm.es:20.500.14352/121476</identifier><datestamp>2025-06-18T23:57:36Z</datestamp><setSpec>com_20.500.14352_14</setSpec><setSpec>col_20.500.14352_15</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>Nd isotopic heterogeneity in late-Hercynian granitic plutons from Central Spain</dc:title>
   <dc:title>Heterogeneidades isotópicas de Nd en plutones graníticos tardi-hercínicos de la región central española</dc:title>
   <dc:creator>Villaseca González, Carlos</dc:creator>
   <dc:creator>Barbero González, Luis C.</dc:creator>
   <dc:creator>Rogers, G.</dc:creator>
   <dc:creator>Reyes Hernández, Javier</dc:creator>
   <dc:creator>Santos Zalduegui, José Francisco</dc:creator>
   <dc:subject>552.3(460)"621.6"</dc:subject>
   <dc:subject>Sr and Nd isotopes</dc:subject>
   <dc:subject>Hercynian granites</dc:subject>
   <dc:subject>Open/closed magnetic processes</dc:subject>
   <dc:subject>Petrología</dc:subject>
   <dc:subject>2506.13 Petrología Ignea y Metamórfica</dc:subject>
   <dc:description>23ª Sesión Científica, Madrid 1997.</dc:description>
   <dc:description>Some Hercynian granitic plutons from Central Spain show variation in initial Nd isotopic ratios defining different trends with increasing silica content. There is a decoupling between the Sr and Nd isotopic systems as these plutons present homogeneous initial Sr ratios. Magmatic processes could explain this Nd isotopic disequilibrium; it is suggested that Nd-bearing restitic or early precipitating accesory phases could control the Nd isotopic heterogeneity of the granites.</dc:description>
   <dc:description>Dirección General de Investigación Científica y Técnica (España)</dc:description>
   <dc:description>Depto. de Mineralogía y Petrología</dc:description>
   <dc:description>Fac. de Ciencias Geológicas</dc:description>
   <dc:description>TRUE</dc:description>
   <dc:description>pub</dc:description>
   <dc:date>2025-06-18T09:52:54Z</dc:date>
   <dc:date>2025-06-18T09:52:54Z</dc:date>
   <dc:date>1997</dc:date>
   <dc:type>journal article</dc:type>
   <dc:type>VoR</dc:type>
   <dc:identifier>https://hdl.handle.net/20.500.14352/121476</dc:identifier>
   <dc:identifier>0213-683X</dc:identifier>
   <dc:language>eng</dc:language>
   <dc:relation>PB93-0295-CO2</dc:relation>
   <dc:relation>Villaseca González, C. et al. (1997) «Nd isotopic heterogeneity in late-Hercynian granitic plutons from Central Spain», Geogaceta, 23, pp. 165-168.</dc:relation>
   <dc:rights>open access</dc:rights>
   <dc:format>application/pdf</dc:format>
   <dc:publisher>Sociedad Geológica de España</dc:publisher>
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