<?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>2026-06-26T20:58:38Z</responseDate><request verb="GetRecord" identifier="oai:docta.ucm.es:20.500.14352/60202" metadataPrefix="mods">https://docta.ucm.es/rest/oai/request</request><GetRecord><record><header><identifier>oai:docta.ucm.es:20.500.14352/60202</identifier><datestamp>2024-07-24T18:17:15Z</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>Lillo Ramos, F. Javier</mods:namePart>
   </mods:name>
   <mods:name>
      <mods:namePart>Oyarzun Muñoz, Roberto</mods:namePart>
   </mods:name>
   <mods:name>
      <mods:namePart>Ortega Menor, Lorena</mods:namePart>
   </mods:name>
   <mods:name>
      <mods:namePart>Gallego, M.</mods:namePart>
   </mods:name>
   <mods:extension>
      <mods:dateAvailable encoding="iso8601">2023-06-20T20:23:30Z</mods:dateAvailable>
   </mods:extension>
   <mods:extension>
      <mods:dateAccessioned encoding="iso8601">2023-06-20T20:23:30Z</mods:dateAccessioned>
   </mods:extension>
   <mods:originInfo>
      <mods:dateIssued encoding="iso8601">1996</mods:dateIssued>
   </mods:originInfo>
   <mods:identifier type="issn">0213-683X</mods:identifier>
   <mods:identifier type="uri">https://hdl.handle.net/20.500.14352/60202</mods:identifier>
   <mods:identifier type="officialurl">http://www.sociedadgeologica.es/publicaciones_geogaceta.html</mods:identifier>
   <mods:abstract>The most outstanding metallogenic period in central Spain took place during the so-cal/ed lateHercynian
episode. This episode was characterized by widespread extensional conditions resulting from
the collapse of an overthickened and overheated Hercynian orogen. A combination of magmatic activity
and favorable structures induced hydrothermal activity leading to Sn-W, Pb-Zn, Ag-base metals, base metals-Ba-(F) and Sb-(Au) deposition. Five ore deposits/districts: El Trasquilón (Sn), Linares-La CarolinaTorrecillas (Pb-Zn-Ba-[Ag]), Sierra de Guadarrama (Ba-(F)-[base metals]), El Juncalón (Sb-[Au]), and Hiendelaencina (Ag-base metals) allow characterization of the main geologic features of this metallogenic episode.</mods:abstract>
   <mods:language>
      <mods:languageTerm>spa</mods:languageTerm>
   </mods:language>
   <mods:accessCondition type="useAndReproduction">open access</mods:accessCondition>
   <mods:titleInfo>
      <mods:title>La actividad metalogénica durante el Tardihercínico en el centro
de España: una visión desde cinco localidades tipo</mods:title>
   </mods:titleInfo>
   <mods:genre>journal article</mods:genre>
</mods:mods></metadata></record></GetRecord></OAI-PMH>