<?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>2026-06-08T11:26:33Z</responseDate><request verb="GetRecord" identifier="oai:docta.ucm.es:20.500.14352/58276" metadataPrefix="marc">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><record xmlns="http://www.loc.gov/MARC21/slim" 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://www.loc.gov/MARC21/slim http://www.loc.gov/standards/marcxml/schema/MARC21slim.xsd">
   <leader>00925njm 22002777a 4500</leader>
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      <subfield code="a">dc</subfield>
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   <datafield ind2=" " ind1=" " tag="720">
      <subfield code="a">Bógalo Román, María Felicidad</subfield>
      <subfield code="e">author</subfield>
   </datafield>
   <datafield ind2=" " ind1=" " tag="720">
      <subfield code="a">Osete López, María Luisa</subfield>
      <subfield code="e">author</subfield>
   </datafield>
   <datafield ind2=" " ind1=" " tag="720">
      <subfield code="a">Ancochea Soto, Eumenio</subfield>
      <subfield code="e">author</subfield>
   </datafield>
   <datafield ind2=" " ind1=" " tag="720">
      <subfield code="a">Villalain, J.J.</subfield>
      <subfield code="e">author</subfield>
   </datafield>
   <datafield ind2=" " ind1=" " tag="260">
      <subfield code="c">1994-06</subfield>
   </datafield>
   <datafield ind2=" " ind1=" " tag="520">
      <subfield code="a">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.</subfield>
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      <subfield code="a">0213-683X</subfield>
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      <subfield code="a">https://hdl.handle.net/20.500.14352/58276</subfield>
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      <subfield code="a">http://www.sociedadgeologica.es/</subfield>
   </datafield>
   <datafield ind2="0" ind1="0" tag="245">
      <subfield code="a">Estudio paleomagnético del volcanismo de Campos de Calatrava</subfield>
   </datafield>
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