<?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>0016-7169</journal-id>
<journal-title><![CDATA[Geofísica internacional]]></journal-title>
<abbrev-journal-title><![CDATA[Geofís. Intl]]></abbrev-journal-title>
<issn>0016-7169</issn>
<publisher>
<publisher-name><![CDATA[Universidad Nacional Autónoma de México, Instituto de Geofísica]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S0016-71692020000100005</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[An intraslab earthquake at a depth of 100 km in the subducting Cocos plate beneath Nevado de Toluca volcano]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Singh]]></surname>
<given-names><![CDATA[Shri K.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Pérez-Campos]]></surname>
<given-names><![CDATA[Xyoli]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Espindola]]></surname>
<given-names><![CDATA[Víctor Hugo]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Iglesias]]></surname>
<given-names><![CDATA[Arturo]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Quintanar]]></surname>
<given-names><![CDATA[Luis]]></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 ]]></institution>
<addr-line><![CDATA[CDMX ]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad Nacional Autónoma de México Instituto de Geofísica Servicio Sismológico Nacional]]></institution>
<addr-line><![CDATA[CDMX ]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Universidad Nacional Autónoma de México Instituto de Geofísica Servicio Sismológico Nacional]]></institution>
<addr-line><![CDATA[CDMX ]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af4">
<institution><![CDATA[,Universidad Nacional Autónoma de México Instituto de Geofísica ]]></institution>
<addr-line><![CDATA[CDMX ]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af5">
<institution><![CDATA[,Universidad Nacional Autónoma de México Instituto de Geofísica Servicio Sismológico Nacional]]></institution>
<addr-line><![CDATA[CDMX ]]></addr-line>
<country>Mexico</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>03</month>
<year>2020</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>03</month>
<year>2020</year>
</pub-date>
<volume>59</volume>
<numero>1</numero>
<fpage>5</fpage>
<lpage>12</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S0016-71692020000100005&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S0016-71692020000100005&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S0016-71692020000100005&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract Seismicity in the subducted Cocos plate below central Mexico, defined by moderate and large earthquakes, ceases well before reaching the active volcanic front. No intraslab earthquake has been reliably located below Nevado de Toluca and Popocatepetl volcanos. Here we report on an M w3.3 event at a depth of 98 km, 38 km to the west of Nevado de Toluca. The event provides evidence, for the first time from an earthquake, of subducted slab at a depth of ~ 100 km below the volcano. Recordings of the event also provide evidence of high attenuation of shear waves as they propagate through the mantle-wedge asthenosphere. It is possible that intraslab seismicity beneath active volcanoes in central Mexico at M ~3 level is abundant but has not been documented in the past because of poor instrumentation.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen La sismicidad en la placa de Cocos subducida por debajo de México central, definida por sismos moderados y grandes, cesa antes de al frente volcánico activo. No se ha localizado algún sismo intraplaca por debajo de los volcanes Nevado de Toluca y Popocatépetl. En este trabajo se reporta un evento de M  w 3.3 a una profundidad de 98 km, a 38 km al oeste del Nevado de Toluca. Este evento provee evidencia, por primera vez, de un sismo en la placa subducida a profundidad de ~100 km por debajo del volcán. Registros de este evento también proveen evidencia de una alta atenución de las ondas de cizalla conforme se propagan a través de la cuña del manto astenosférico. Es posible que la sismicidad intraplaca por debajo de los volcanes activos en México central, a un nivel de M ~3, sea abundante pero que no ha sido documentada en el pasado por la falta de instrumentación en la región.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[sismicidad intraplaca]]></kwd>
<kwd lng="es"><![CDATA[Nevado de Toluca]]></kwd>
<kwd lng="es"><![CDATA[mando astenosférico]]></kwd>
<kwd lng="es"><![CDATA[México]]></kwd>
<kwd lng="en"><![CDATA[intraplate seismicity]]></kwd>
<kwd lng="en"><![CDATA[Nevado de Toluca]]></kwd>
<kwd lng="en"><![CDATA[asthenospheric control]]></kwd>
<kwd lng="en"><![CDATA[Mexico]]></kwd>
</kwd-group>
</article-meta>
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