<?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>1993-8012</journal-id>
<journal-title><![CDATA[Minería y Geología]]></journal-title>
<abbrev-journal-title><![CDATA[Min. Geol.]]></abbrev-journal-title>
<issn>1993-8012</issn>
<publisher>
<publisher-name><![CDATA[EDUM. Universidad de Moa]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S1993-80122021000200130</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Comportamiento de la actividad sísmica anómala iniciada el 17 de enero de 2016 al sur de Santiago de Cuba]]></article-title>
<article-title xml:lang="en"><![CDATA[Anomalous seismic activity performance in January 17/ 2016 in southern part of Santiago de Cuba]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[González-Matos]]></surname>
<given-names><![CDATA[O&#8217;Leary Fernando]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Arango-Arias]]></surname>
<given-names><![CDATA[Enrique Diego]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Moreno-Toirán]]></surname>
<given-names><![CDATA[Bladimir]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Leyva-Arias]]></surname>
<given-names><![CDATA[Maribel]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Berenguer-Heredia]]></surname>
<given-names><![CDATA[Yelena]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Centro Nacional de Investigaciones Sismológicas  ]]></institution>
<addr-line><![CDATA[ Santiago de Cuba]]></addr-line>
<country>Cuba</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>06</month>
<year>2021</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>06</month>
<year>2021</year>
</pub-date>
<volume>37</volume>
<numero>2</numero>
<fpage>130</fpage>
<lpage>145</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://scielo.sld.cu/scielo.php?script=sci_arttext&amp;pid=S1993-80122021000200130&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://scielo.sld.cu/scielo.php?script=sci_abstract&amp;pid=S1993-80122021000200130&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://scielo.sld.cu/scielo.php?script=sci_pdf&amp;pid=S1993-80122021000200130&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen Se evaluó comportamiento y las posibles causas de la actividad sísmica al sur de la provincia de Santiago de Cuba, a partir de la información geológica y tectónica disponible y de los registros de los sismos ocurridos en esta región desde el 17 de enero del 2016 a las 08:17 UTC. El análisis de los parámetros espacio-temporal-energéticos de los terremotos evidenció la coherencia entre los resultados de tres de las redes que monitorean la región, a saber, Servicio Sismológico Nacional Cubano (SSNC), Servicio Geológico de los Estados Unidos (USGS) y el Centro Alemán de Investigaciones Geocientíficas (GEOFON)). Para tres de los terremotos se calcularon los tensores del momento sísmico mediante el proceso de inversión de las correspondientes formas de ondas. La comparación de los resultados de dos de ellos con los obtenidos por otras agencias que monitorean el área fue totalmente coherente con planos de fallas de orientación N-S con mecanismos focales compresivos. El tercer sismo, ocurrido una semana más tarde al este de la provincia, también tuvo un mecanismo compresivo, aunque con orientación NW-SE en el plano de falla. La actividad sísmica que en sus inicios se comportó como un enjambre de terremotos, manifestó posteriormente un comportamiento distinto, similar al de réplicas registradas tras un sismo de mayor energía, siguiendo la Ley de Omori, es decir, del tipo de evento premonitores-sismo principal-replicas.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT Performance and possible causes of seismic activity in the southern of Santiago de Cuba province were evaluated, based on the geological and tectonic information available and records of the earthquakes occurred in this region in January 17, 2016 at 08:17 UTC. The analysis of the space-time-energy parameters of the earthquakes showed the coherence between the results of three of the networks monitoring the region, namely, the Cuban National Seismological Service (SSNC), the United States Geological Service (USGS) and the German Center for Geo-scientific Research (GEOFON)). For three of the earthquakes, the seismic moment tensors were calculated by reversing the corresponding waveforms. Comparing the results of two of them with those obtained by other agencies that monitor the area was totally consistent with fault planes oriented N-S with compressive focal mechanisms. The third earthquake, which occurred a week later in the east of the province, also had a compressive mechanism, although with a NW-SE orientation on the fault plane. The seismic activity that initially performed like a swarm of earthquakes, performed differently later; similar to aftershocks registered after a higher-energy earthquake, following Omori's Law, that is, the type of premonitory-main earthquake event -aftershocks.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[sismicidad]]></kwd>
<kwd lng="es"><![CDATA[réplicas]]></kwd>
<kwd lng="es"><![CDATA[Santiago de Cuba]]></kwd>
<kwd lng="es"><![CDATA[tensor del momento sísmico]]></kwd>
<kwd lng="es"><![CDATA[ángulo de Kagan]]></kwd>
<kwd lng="en"><![CDATA[seismic activity]]></kwd>
<kwd lng="en"><![CDATA[aftershocks]]></kwd>
<kwd lng="en"><![CDATA[Santiago de Cuba]]></kwd>
<kwd lng="en"><![CDATA[seismic moment tensor]]></kwd>
<kwd lng="en"><![CDATA[Kagan angle]]></kwd>
</kwd-group>
</article-meta>
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