<?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>2026-06-29T08:21:24Z</responseDate><request verb="GetRecord" identifier="oai:docta.ucm.es:20.500.14352/8620" metadataPrefix="oai_dc">https://docta.ucm.es/rest/oai/request</request><GetRecord><record><header><identifier>oai:docta.ucm.es:20.500.14352/8620</identifier><datestamp>2023-08-25T23:54:58Z</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>Age and petrogenesis of the beryl-bearing granitic magmatism of the Velasco Pegmatite District, Pampeana Province, NW Argentina</dc:title>
   <dc:creator>Sardi, Fernando Guillermo</dc:creator>
   <dc:creator>Marangone, Silvana</dc:creator>
   <dc:creator>Fuenlabrada Pérez, José Manuel</dc:creator>
   <dc:subject>552.3(823.1)</dc:subject>
   <dc:subject>Rb-Sr isochron</dc:subject>
   <dc:subject>petrogenesis</dc:subject>
   <dc:subject>pegmatite</dc:subject>
   <dc:subject>Velasco District</dc:subject>
   <dc:subject>Pampean Pegmatite Province</dc:subject>
   <dc:subject>Geoquímica</dc:subject>
   <dc:subject>Petrología</dc:subject>
   <dc:subject>2503 Geoquímica</dc:subject>
   <dc:description>Two porphyritic granitoids (Huaco and Sanagasta) in the Velasco district of the Pampeana Pegmatite Province in Northwestern Argentina are recognized. They are considered the fertile granites of the beryl-bearing pegmatites and can be described as post-orogenic and peraluminous A-type granites formed in an intraplate tectonic setting during an extensive regime, whose magma source is predominantly of cortical origin and to a lesser extent, mantle-derived. The pegmatites are classified as Rare Elements of the beryl type and beryl-columbite-phosphate subtype, while the entire district shows characteristics related to the NYF (Nb-Y-F) petrogenetic family. From rocks and cogenetic minerals of an individual ‘Ismiango’ pegmatite of the Velasco district, two Rb/Sr isochrons have been constructed. They define an age of 330.3 ± 8.3 and 331.7 ± 2.3 Ma and fall in the Lower Carboniferous period, consistent with the age of the parental and host-rock, the Huaco granite. As the Ismiango pegmatite has a similar composition and structure to the other beryl mineralized pegmatites of the Velasco district, the obtained age is attributed extensively for the entire district. According to the initial 87Sr/86Sr value obtained of 0.713, the pegmatite-magmatism of the Velasco District might be mainly derived from the crust with some minor participation of mantle materials.</dc:description>
   <dc:description>Consejo Nacional de Investigaciones Científicas y Tecnológicas  (CONICET, Argentina).</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>2023-06-17T09:20:15Z</dc:date>
   <dc:date>2023-06-17T09:20:15Z</dc:date>
   <dc:date>2021</dc:date>
   <dc:type>journal article</dc:type>
   <dc:identifier>https://hdl.handle.net/20.500.14352/8620</dc:identifier>
   <dc:identifier>2317-4889</dc:identifier>
   <dc:identifier>10.1590/2317-4889202120210030</dc:identifier>
   <dc:language>eng</dc:language>
   <dc:relation>PIP 642</dc:relation>
   <dc:rights>Atribución 3.0 España</dc:rights>
   <dc:rights>https://creativecommons.org/licenses/by/3.0/es/</dc:rights>
   <dc:rights>open access</dc:rights>
   <dc:format>application/pdf</dc:format>
   <dc:publisher>Sociedade Brasileira de Geologia</dc:publisher>
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