<?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>2026-06-08T09:51:23Z</responseDate><request verb="GetRecord" identifier="oai:docta.ucm.es:20.500.14352/58276" metadataPrefix="mods">https://docta.ucm.es/rest/oai/request</request><GetRecord><record><header><identifier>oai:docta.ucm.es:20.500.14352/58276</identifier><datestamp>2024-08-29T16:59:07Z</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>Bógalo Román, María Felicidad</mods:namePart>
   </mods:name>
   <mods:name>
      <mods:namePart>Osete López, María Luisa</mods:namePart>
   </mods:name>
   <mods:name>
      <mods:namePart>Ancochea Soto, Eumenio</mods:namePart>
   </mods:name>
   <mods:name>
      <mods:namePart>Villalain, J.J.</mods:namePart>
   </mods:name>
   <mods:extension>
      <mods:dateAvailable encoding="iso8601">2023-06-20T17:28:10Z</mods:dateAvailable>
   </mods:extension>
   <mods:extension>
      <mods:dateAccessioned encoding="iso8601">2023-06-20T17:28:10Z</mods:dateAccessioned>
   </mods:extension>
   <mods:originInfo>
      <mods:dateIssued encoding="iso8601">1994-06</mods:dateIssued>
   </mods:originInfo>
   <mods:identifier type="issn">0213-683X</mods:identifier>
   <mods:identifier type="uri">https://hdl.handle.net/20.500.14352/58276</mods:identifier>
   <mods:identifier type="officialurl">http://www.sociedadgeologica.es/</mods:identifier>
   <mods:abstract>A first systematic paleomagnetic study has been carried out in the upper Miocene-Pliocene volcanísm
of the Campos de Calatrava region. 78 localities have been sampled and 74 oi them yíelded useiul
paleomagnetíc results. A Pliocene paleomagnetic pole has been obtaíned for the {be rían Plate (Lat.=
82.7°N, Long.= 771.6°E, A95= 6.9). On the basis of the magnetíc polarity results a zoníng oi the
voJcanism may be recognízed which could be explaíned by a NE-wardmigration of the volcanism in
thís regíon.</mods:abstract>
   <mods:language>
      <mods:languageTerm>spa</mods:languageTerm>
   </mods:language>
   <mods:accessCondition type="useAndReproduction">open access</mods:accessCondition>
   <mods:titleInfo>
      <mods:title>Estudio paleomagnético del volcanismo de Campos de Calatrava</mods:title>
   </mods:titleInfo>
   <mods:genre>journal article</mods:genre>
</mods:mods></metadata></record></GetRecord></OAI-PMH>