<?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>0256-7024</journal-id>
<journal-title><![CDATA[Revista Geológica de América Central]]></journal-title>
<abbrev-journal-title><![CDATA[Rev. Geol. Amér. Central]]></abbrev-journal-title>
<issn>0256-7024</issn>
<publisher>
<publisher-name><![CDATA[Universidad de Costa Rica]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S0256-70242021000200142</article-id>
<article-id pub-id-type="doi">10.15517/rgac.v0i65.47012</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Análisis retrospectivo del terremoto de Limón del 22 de abril de 1991 (Mw 7,7) y de la actividad sísmica disparada en las fallas Ayil, Pacuare, Atirro, División y Navarro]]></article-title>
<article-title xml:lang="en"><![CDATA[Retrospective analysis of the Limón earthquake of April 22, 1991 (Mw 7.7) and its triggered seismicity in the Ayil, Pacuare, Atirro, División and Navarro faults]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Montero-Pohly]]></surname>
<given-names><![CDATA[Walter]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad de Costa Rica Centro de Investigaciones en Ciencias Geológicas ]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
<country>Costa Rica</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>12</month>
<year>2021</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>12</month>
<year>2021</year>
</pub-date>
<numero>65</numero>
<fpage>142</fpage>
<lpage>168</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.sa.cr/scielo.php?script=sci_arttext&amp;pid=S0256-70242021000200142&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.sa.cr/scielo.php?script=sci_abstract&amp;pid=S0256-70242021000200142&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.sa.cr/scielo.php?script=sci_pdf&amp;pid=S0256-70242021000200142&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen Datos de sismicidad, sismotectónicos y neotectónicos permiten realizar un análisis retrospectivo del terremoto de Limón del 22 de abril de 1991 (Mw 7,7) y de la actividad de réplicas y la disparada. Se revisan el área sísmica de la ruptura, y los modelos de inversión, con los cuales se obtuvieron el mecanismo focal y el momento sísmico. Diversos estudios concluyen que el evento principal se originó en una falla inversa de bajo ángulo inclinada al suroeste, localizada en la Baja Talamanca, debido al sobrecorrimiento del bloque de Panamá sobre la placa Caribe. El análisis de la sismicidad disparada y de su sismotectónica determinan que las fallas dextrales Ayil, Pacuare y Atirro y las sinestrales División y Navarro fueron reactivadas por este terremoto. Estas fallas se ubican en el Cinturón Deformado del Centro de Costa Rica y en la zona de transición con el sector oeste del Cinturón Deformado del Norte de Panamá.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract A retrospective analysis of the April 22, 1991 Limón earthquake (Mw 7.7) and of its aftershock and triggered activity is performed using seismicity, seismotectonic and neotectonic data. The seismic rupture area is reviewed as well as inversion models that allow to obtain the focal mechanism, and seismic moment. Different studies confirm that the mainshock source was a low angle thrust fault dipping southwest located in the back-arc region of the Talamanca Cordillera. The fault overthrusts the Panama block over the Caribbean plate. The analysis of the triggered seismicity and its seismotectonics show that the right-lateral Ayil, Pacuare and Atirro faults and the División and Navarro left-lateral faults were reactivated by the Limón earthquake. These faults are located along the Central Costa Rica Deformed Belt and in the transition zone with the western border of the North Panama Deformed Belt.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[Seismicity]]></kwd>
<kwd lng="en"><![CDATA[Seismotectonics]]></kwd>
<kwd lng="en"><![CDATA[Neotectonics]]></kwd>
<kwd lng="en"><![CDATA[Central Costa Rica Deformed Belt]]></kwd>
<kwd lng="en"><![CDATA[North Panama Deformed Belt.]]></kwd>
<kwd lng="es"><![CDATA[Sismicidad]]></kwd>
<kwd lng="es"><![CDATA[Sismotectónica]]></kwd>
<kwd lng="es"><![CDATA[Neotectónica]]></kwd>
<kwd lng="es"><![CDATA[Cinturón Deformado del Centro de Costa Rica]]></kwd>
<kwd lng="es"><![CDATA[Cinturón Deformado del Norte de Panamá.]]></kwd>
</kwd-group>
</article-meta>
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