<?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>S0016-71692017000300255</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[Paleoseismological uncertainty estimation in the Acambay region, Central Mexico]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Rodríguez-Pérez]]></surname>
<given-names><![CDATA[Quetzalcoatl]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Zúñiga]]></surname>
<given-names><![CDATA[F. Ramón]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Lacan]]></surname>
<given-names><![CDATA[Pierre]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Consejo Nacional de Ciencia y Tecnología Dirección Adjunta de Desarrollo Científico Dirección de Cátedras]]></institution>
<addr-line><![CDATA[Ciudad de México ]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad Nacional Autónoma de México Centro de Geociencias ]]></institution>
<addr-line><![CDATA[Juriquilla Querétaro]]></addr-line>
<country>Mexico</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>09</month>
<year>2017</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>09</month>
<year>2017</year>
</pub-date>
<volume>56</volume>
<numero>3</numero>
<fpage>255</fpage>
<lpage>268</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S0016-71692017000300255&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S0016-71692017000300255&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S0016-71692017000300255&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract: Paleseismological studies provide valuable information of the earthquake rupture processes such as fault dimensions, average and maximum displacements, as well as recurrence times and magnitudes of events which took place in the geologic past. This information is based on geological observations record. Interpretation of geological observations has a source of uncertainties inherent to the large number of hypothesis that explain the observed geological features. Information obtained from paleoseismic studies is important in seismic hazard analyses, and particularly crucial for regions of low seismic activity where the recurrence period of major earthquakes reaches several thousand years. However, using this information in hazard analysis requires the systematic treatment of uncertainties. We estimated uncertainties of four paleoseismological studies conducted at three different faults of the Acambay graben region in Central Mexico. The method used is based on a logic-tree formalism that quantifies the cumulative uncertainties associated with the different stages of the paleoseismic studies together with a quantification of the entropy at each step and at the end of the process. The final uncertainty and its relative importance is seismic hazard analysis is expressed as the paleoseismic quality factor, which indicate 0.14, 0.40-0.50, and 0.41 for the AcambayTixmadejé, Pastores and San Mateo faults, respectively. These values can be incorporated in seismic hazard analyses for the region.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen: Los estudios paleosismológicos proporcionan información valiosa de los procesos de ruptura de los terremotos como son: las dimensiones de las fallas geológicas, los desplazamientos promedios y máximos, así como los tiempos de recurrencia y las magnitudes de eventos ocurridos en el pasado geológico. Esta información se basa en observaciones en los registros geológicos. La interpretación de dichas observaciones geológicas tienen una fuente de incertidumbres inherente al gran número de hipótesis que explican las características geológicas observadas. La información obtenida a partir de estudios paleosísmicos es importante en el análisis del riesgo sísmico y es crucial sobre todo para las regiones de baja actividad sísmica en donde el tiempo de recurrencia de los terremotos mayores alcanzan varios miles de años. Sin embargo, el uso de esta información en el análisis de riesgos requiere un tratamiento sistemático de las incertidumbres. En este estudio, se estimaron las incertidumbres de cuatro estudios paleosismológicos realizados en tres fallas geológicas diferentes en la región del graben de Acambay en el Centro de México. El método usado se basa en el formalismo de los árboles lógicos que cuantifica las incertidumbres acumuladas asociadas con las diferentes etapas de los estudios paleosismológicos aunado a una evaluación de la entropía en cada paso y al final del proceso. La incertidumbre final y su importancia relativa en el análisis de riesgo sísmico se expresa como el factor de calidad paleosísmico, el cuál es de 0.14, 0.40-0.50 y 0.41 para las fallas de Acambay-Tixmadeje, Pastores y San Mateo, respectivamente. Estos valores se pueden incorporar en los análisis de riesgo sísmico para la región.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[Eje Neovolcánico]]></kwd>
<kwd lng="es"><![CDATA[Acambay]]></kwd>
<kwd lng="es"><![CDATA[Paleosismología]]></kwd>
<kwd lng="es"><![CDATA[incertidumbres]]></kwd>
<kwd lng="es"><![CDATA[riesgo sísmico]]></kwd>
<kwd lng="es"><![CDATA[árbol lógico]]></kwd>
<kwd lng="en"><![CDATA[Trans-Mexican Volcanic Belt]]></kwd>
<kwd lng="en"><![CDATA[Acambay]]></kwd>
<kwd lng="en"><![CDATA[Paleoseismology]]></kwd>
<kwd lng="en"><![CDATA[uncertainties]]></kwd>
<kwd lng="en"><![CDATA[seismic risk]]></kwd>
<kwd lng="en"><![CDATA[logic-tree]]></kwd>
</kwd-group>
</article-meta>
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