<?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>S0016-71692024000401165</article-id>
<article-id pub-id-type="doi">10.22201/igeof.2954436xe.2024.63.4.1773</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Análisis mediante estadística no extensiva del terremoto de Pedernales, Ecuador 2016]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Barahona Cárdenas]]></surname>
<given-names><![CDATA[Daniel Andrés]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Araujo Soria]]></surname>
<given-names><![CDATA[José Sebastián]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad Regional Amazo&#769;nica Ikiam Facultad de Ciencias de la Tierra y Agua ]]></institution>
<addr-line><![CDATA[Tena ]]></addr-line>
<country>Ecuador</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad Regional Amazo&#769;nica Ikiam Facultad de Ciencias de la Tierra y Agua ]]></institution>
<addr-line><![CDATA[Tena ]]></addr-line>
<country>Ecuador</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>12</month>
<year>2024</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>12</month>
<year>2024</year>
</pub-date>
<volume>63</volume>
<numero>4</numero>
<fpage>1165</fpage>
<lpage>1174</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S0016-71692024000401165&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S0016-71692024000401165&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S0016-71692024000401165&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen El 16 de abril de 2016 ocurrió un terremoto en Ecuador de magnitud 7.8 el cual causó enormes pérdidas humanas y materiales, y miles de personas heridas y desplazadas. Este evento sísmico forma parte de un conjunto de sismos en la provincia de Manabí en la región costera de Ecuador donde se produce la subducción de la placa de Nazca bajo la placa Sudamericana. Proponemos estudiar este conjunto de sismos desde la perspectiva de la mecánica estadística no extensiva utilizando el concepto de entropía propuesta por Tsallis en (Tsallis, 2009). Desarrollamos el cálculo del coeficiente de complejidad q para la magnitud de los sismos, parámetro que cuantifica el valor de complejidad de un sistema, y lo aplicamos al catálogo de terremotos en la zona de alto acoplamiento sísmico de Manabí-Esmeraldas en la zona de subducción de Ecuador. Los resultados muestran una relación entre los cambios en el coeficiente de complejidad q a través del tiempo y la ocurrencia de sismos de gran magnitud M&gt;5. El terremoto del 16 de abril de 2016 acompaña un previo incremento en el valor de q el cual coincide con otros estudios anteriores como en (Papadakis et al., 2015).]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract On April 16, 2016, a magnitude 7.8 earthquake occurred in Ecuador, causing enormous human and material losses, and leaving thousands of people injured and displaced. This seismic event is part of a series of earthquakes in the province of Manabí in the coastal region of Ecuador, where the subduction of the Nazca plate under the South American plate occurs. We propose to study this set of earthquakes from the perspective of non-extensive statistical mechanics using the entropy concept proposed by Tsallis in (Tsallis, 2009). We developed the calculation of the complexity coefficient q for the magnitude of earthquakes, a parameter that quantifies the value of complexity of a system, and applied it to the earthquake catalog in the high seismic coupling zone of Manabí-Esmeraldas in the subduction zone of Ecuador. The results show a relationship between changes in the complexity coefficient q over time and the occurrence of earthquakes of great magnitude M&gt;5. The earthquake of April 16, 2016, is accompanied by a previous increase in the value of q, which coincides with other previous studies such as in (Papadakis et al., 2015).]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[Terremoto]]></kwd>
<kwd lng="es"><![CDATA[Manabí]]></kwd>
<kwd lng="es"><![CDATA[complejidad]]></kwd>
<kwd lng="es"><![CDATA[no extensividad]]></kwd>
<kwd lng="es"><![CDATA[entropía]]></kwd>
<kwd lng="en"><![CDATA[Earthquake]]></kwd>
<kwd lng="en"><![CDATA[Manabí]]></kwd>
<kwd lng="en"><![CDATA[complexity]]></kwd>
<kwd lng="en"><![CDATA[non-extensivity]]></kwd>
<kwd lng="en"><![CDATA[entropy]]></kwd>
</kwd-group>
</article-meta>
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