<?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>2026-06-07T15:51:05Z</responseDate><request verb="GetRecord" identifier="oai:docta.ucm.es:20.500.14352/71308" metadataPrefix="qdc">https://docta.ucm.es/rest/oai/request</request><GetRecord><record><header><identifier>oai:docta.ucm.es:20.500.14352/71308</identifier><datestamp>2023-07-13T02:31:13Z</datestamp><setSpec>com_20.500.14352_14</setSpec><setSpec>col_20.500.14352_15</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>The unique Cambro-Ordovician silicic large igneous province of NW Gondwana: Catastrophic melting of a thinned crust</dc:title>
   <dc:creator>Rodríguez, Carmen</dc:creator>
   <dc:creator>Castro, Antonio</dc:creator>
   <dc:creator>Gómez Frutos, Daniel</dc:creator>
   <dc:creator>Gutiérrez Alonso, Gabriel</dc:creator>
   <dc:creator>Pereira, Manuel Francisco</dc:creator>
   <dc:creator>Fernández, Carlos</dc:creator>
   <dcterms:abstract>Cambro–Ordovician silicic magmatism in the Central Iberian Zone of the Iberian Massif (Ollo de Sapo Formation, OSF) constitutes a voluminous and geochemically atypical magmatic event that formed preceding the breakup of the northern margin of Gondwana. To date, and due to uncommon geochemical signatures, such as a high Fe, Mg content compared to anatectic melts and the departing from the calc-alkaline trends, the origin of such magmatic event is not fully understood. Herein, we report a data-analysis of geochemistry linking magmas and source compositions. The analysis of the combined data from multiple studies ascribes the geochemistry of the OSF rocks to a combination of extensive melting of Ediacaran metasiliciclastic rocks and a Ca-rich component. It is hypothesized that fluids released by crystallization of mafic magmas contributed to partial melting of a thick metasedimentary pile represented by Ediacaran siliciclastic rocks. Such melting event gave rise to a mobile nebulite or migma, which was able to extrude and form the super-eruption or “flare-up” that characterizes Cambro-Ordovician silicic magmatism at the Gondwana margin. Fast, catastrophic crustal melting with large-scale restite entrainment, triggered by the influx of mafic magma-derived fluids, are considered the main cause of the unique features of this Cambro-Ordovician atypical silicic large igneous province of Gondwana.</dcterms:abstract>
   <dcterms:dateAccepted>2023-06-22T10:40:32Z</dcterms:dateAccepted>
   <dcterms:available>2023-06-22T10:40:32Z</dcterms:available>
   <dcterms:created>2023-06-22T10:40:32Z</dcterms:created>
   <dcterms:issued>2022-02-03</dcterms:issued>
   <dc:type>journal article</dc:type>
   <dc:identifier>https://hdl.handle.net/20.500.14352/71308</dc:identifier>
   <dc:identifier>1342-937X</dc:identifier>
   <dc:identifier>10.1016/j.gr.2022.01.011</dc:identifier>
   <dc:language>eng</dc:language>
   <dc:relation>IBERCRUST (PGC2018-096534-B-I00)</dc:relation>
   <dc:relation>UIDB/04683/2020</dc:relation>
   <dc:rights>https://creativecommons.org/licenses/by-nc-nd/3.0/es/</dc:rights>
   <dc:rights>open access</dc:rights>
   <dc:rights>Atribución-NoComercial-SinDerivadas 3.0 España</dc:rights>
   <dc:publisher>Elsevier</dc:publisher>
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