<?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>S0256-70242021000200169</article-id>
<article-id pub-id-type="doi">10.15517/rgac.v0i65.47079</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Terremoto del Valle de La Estrella: análisis sísmico, cascada de desastres y pérdidas económicas en valor presente (2020)]]></article-title>
<article-title xml:lang="en"><![CDATA[Valle de La Estrella earthquake: seismic analysis, disaster cascade and update of economic losses in present value (2020)]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Campos-Durán]]></surname>
<given-names><![CDATA[Daniela]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Quintero-Quintero]]></surname>
<given-names><![CDATA[Ronnie]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Abarca-Rojas]]></surname>
<given-names><![CDATA[Tatiana]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad Nacional (UNA), Escuela de Ciencias Geográficas ]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
<country>Costa Rica</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad Nacional (UNA), Observatorio Vulcanológico y Sismológico de Costa Rica (Ovsicori), ]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
<country>Costa Rica</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Universidad de Costa Rica (UCR), Maestría Profesional en Gestión del Riesgo y Atención de Emergencias ]]></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>169</fpage>
<lpage>192</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.sa.cr/scielo.php?script=sci_arttext&amp;pid=S0256-70242021000200169&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.sa.cr/scielo.php?script=sci_abstract&amp;pid=S0256-70242021000200169&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.sa.cr/scielo.php?script=sci_pdf&amp;pid=S0256-70242021000200169&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen La sismicidad y mecanismos focales en el Cinturón Deformado del Norte de Panamá (CDNP) indican un entorno compresivo asociado al cabalgamiento del Bloque de Panamá (BP) sobre la placa Caribe; mecanismos focales corticales de cizalla en BP se observan en la cordillera de Talamanca y en la Cordillera Volcánica Central. Los hipocentros alcanzan profundidades máximas entre 50-60 km al pie de la cordillera de Talamanca y más superficiales cerca de la costa Caribe. El terremoto del Valle de La Estrella de 1991 (Mw 7,6) disparó réplicas en un área de ~140x70 km; los deslizamientos y licuefacción fueron los eventos secundarios que causaron más daños y pérdidas en infraestructura (vivienda, puentes, red ferroviaria, red vial y acueductos), sus efectos se concentraron en ciudades costeras, como Limón y Bocas del Toro. Las pérdidas económicas de la época en valor presente al 2020 corresponden a $3 433 266 937,41.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract Seismicity and focal mechanisms in the of North Panama Deformed Belt (NPDB) indicate a compressional environment associated with the overthrusting of the Panama Block (PB) on the Caribbean plate; crustal PB strike-slip focal mechanisms are observed in the Talamanca and Central Volcanic Cordillera. The hypocenters reach maximum depths between 50-60 km at the foot of the Talamanca mountain range and are shallow near the Caribbean coast. The 1991, Valle de la Estrella earthquake (Mw 7.6) triggered aftershocks in an area of ~140x70 km; landslides and liquefaction were the secondary events that caused most damage and losses in infrastructure (housing, bridges, railroad network, road network and aqueducts); its effects were concentrated in coastal cities, such as Limón and Bocas del Toro. The economic losses in present 2020 value correspond to $3 433 266 937.41.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[Earthquake]]></kwd>
<kwd lng="en"><![CDATA[Limon]]></kwd>
<kwd lng="en"><![CDATA[1991]]></kwd>
<kwd lng="en"><![CDATA[Liquefaction]]></kwd>
<kwd lng="en"><![CDATA[Landslides]]></kwd>
<kwd lng="en"><![CDATA[Focal Mechanisms]]></kwd>
<kwd lng="en"><![CDATA[South Caribbean]]></kwd>
<kwd lng="es"><![CDATA[Terremoto]]></kwd>
<kwd lng="es"><![CDATA[Limón]]></kwd>
<kwd lng="es"><![CDATA[1991]]></kwd>
<kwd lng="es"><![CDATA[licuefacción]]></kwd>
<kwd lng="es"><![CDATA[deslizamientos]]></kwd>
<kwd lng="es"><![CDATA[mecanismos focales]]></kwd>
<kwd lng="es"><![CDATA[Caribe Sur]]></kwd>
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</article-meta>
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