<?xml version="1.0" encoding="ISO-8859-1"?><article xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance">
<front>
<journal-meta>
<journal-id>1026-8774</journal-id>
<journal-title><![CDATA[Revista mexicana de ciencias geológicas]]></journal-title>
<abbrev-journal-title><![CDATA[Rev. mex. cienc. geol]]></abbrev-journal-title>
<issn>1026-8774</issn>
<publisher>
<publisher-name><![CDATA[Universidad Nacional Autónoma de México, Instituto de Geología]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S1026-87742021000300259</article-id>
<article-id pub-id-type="doi">10.22201/cgeo.20072902e.2021.3.1671</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Revisión de datos paleomagnéticos de flujos de lava asociados al Campo Volcánico Michoacán-Guanajuato: implicaciones sobre el comportamiento del campo magnético terrestre durante el Plio-Cuaternario]]></article-title>
<article-title xml:lang="en"><![CDATA[Review of paleomagnetic data from lava flows associated with the Michoacán-Guanajuato Volcanic Field: implications on the behavior of the Earth&#8217;s magnetic field during the Plio-Quaternary]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Díaz-Ortega]]></surname>
<given-names><![CDATA[Ulises]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[García-Ruiz]]></surname>
<given-names><![CDATA[Rafael]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Cervantes-Solano]]></surname>
<given-names><![CDATA[Miguel]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Goguitchaichvili]]></surname>
<given-names><![CDATA[Avto]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Maciel-Peña]]></surname>
<given-names><![CDATA[Rafael]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Morales-Contreras]]></surname>
<given-names><![CDATA[Juan]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Cejudo-Ruiz]]></surname>
<given-names><![CDATA[Rubén]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad Nacional Autónoma de México Instituto de Geofísica Unidad Michoacán Laboratorio Interinstitucional de Magnetismo Natural]]></institution>
<addr-line><![CDATA[Morelia Mich.]]></addr-line>
<country>Mexico</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>00</month>
<year>2021</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>00</month>
<year>2021</year>
</pub-date>
<volume>38</volume>
<numero>3</numero>
<fpage>259</fpage>
<lpage>271</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1026-87742021000300259&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1026-87742021000300259&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1026-87742021000300259&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen La disponibilidad de edades radiométricas para el Campo Volcánico Michoacán-Guanajuato permite obtener un registro detallado de las variaciones del campo magnético de la Tierra durante los últimos 5 Ma. En el presente trabajo, analizamos 112 direcciones paleomagnéticas confiables respaldadas por igual número de edades radiométricas absolutas. Luego de descartar las polaridades geomagnéticas transicionales siguiendo el criterio de paleolatitudes menores a 45°, se calcularon las direcciones paleomagnéticas medias globales. En términos generales, se observa que la dirección media concuerda, dentro del intervalo de incertidumbres, con las direcciones paleomagnéticas esperadas obtenidas según los polos de referencia Plioceno-Cuaternario. La tasa de variación secular, estimada a través de la dispersión de los polos geomagnéticos virtuales calculados, y la anomalía de inclinación coinciden con los modelos de distribución latitudinal reportados para la latitud de 20° N. Un hallazgo interesante, resultado de esta compilación de direcciones paleomagnéticas, es la posible evidencia de eventos geomagnéticos relativamente cortos o excursiones dentro de los Crones de Matuyama y Brunhes, los cuales pueden ayudar a refinar la escala de tiempo de inestabilidad geomagnética. Además, se presenta una compilación inédita y una descripción minuciosa de más de 1000 aparatos volcánicos realizada por el Dr. Víctor Hugo Garduño Monroy que, sin duda alguna, servirá como una guía para los estudios paleomagnéticos durante las siguientes décadas.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract The great availability of radiometric ages for the Michoacán-Guanajuato Volcanic Field allows obtaining a detailed record of the Earth's magnetic field variations during the last 5 Ma. In this work, we analyze 112 reliable paleomagnetic directions supported by the same number of absolute ages. After discarding the transitional geomagnetic polarities, following the criterion of paleolatitudes less than 45°, the global mean paleomagnetic directions were calculated. In general terms, it is observed that the mean direction agrees, within the uncertainty interval, with the expected paleomagnetic directions obtained according to the Pliocene-Quaternary reference poles. The secular variation rate, estimated through the dispersion of the calculated virtual geomagnetic poles, and the inclination anomaly coincide with the latitudinal distribution models reported for the latitude of 20° N. An interesting finding, resulting from this compilation of paleomagnetic directions, is the possible evidence of relatively short geomagnetic events or excursions within the Matuyama and Brunhes chrones, which may help to refine the geomagnetic instability time scale. Moreover, an unpublished compilation and a detailed description of more than 1000 volcanic buildings by Dr. Víctor Hugo Garduño Monroy are presented, which will undoubtedly serve as an authentic guide for paleomagnetic studies during the following decades.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[Campo Volcánico Michoacán-Guanajuato]]></kwd>
<kwd lng="es"><![CDATA[paleomagnetismo]]></kwd>
<kwd lng="es"><![CDATA[variación paleosecular]]></kwd>
<kwd lng="es"><![CDATA[eventos geomagnéticos cortos]]></kwd>
<kwd lng="es"><![CDATA[México]]></kwd>
<kwd lng="en"><![CDATA[Michoacán-Guanajuato Volcanic Field]]></kwd>
<kwd lng="en"><![CDATA[paleomagnetism]]></kwd>
<kwd lng="en"><![CDATA[paleosecular variation]]></kwd>
<kwd lng="en"><![CDATA[short geomagnetic events]]></kwd>
<kwd lng="en"><![CDATA[Mexico]]></kwd>
</kwd-group>
</article-meta>
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