<?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>S0256-70242016000100179</article-id>
<article-id pub-id-type="doi">10.15517/rgac.v54i0.23283</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Modelo mínimo unidimensional de velocidades de la onda P para la Cordillera Volcánica de Guanacaste, Costa Rica]]></article-title>
<article-title xml:lang="en"><![CDATA[Minimum 1D P wave velocity model for the Guanacaste Volcanic Arc, Costa Rica]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Araya]]></surname>
<given-names><![CDATA[María C.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Linkimer]]></surname>
<given-names><![CDATA[Lepolt]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Taylor]]></surname>
<given-names><![CDATA[Waldo]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad de Costa Rica Escuela Centroamericana de Geología ]]></institution>
<addr-line><![CDATA[San Pedro ]]></addr-line>
<country>CR</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad de Costa Rica Escuela Centroamericana de Geología ]]></institution>
<addr-line><![CDATA[San Pedro ]]></addr-line>
<country>CR</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Universidad de Costa Rica Escuela Centroamericana de Geología ]]></institution>
<addr-line><![CDATA[ San José]]></addr-line>
<country>CR</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>06</month>
<year>2016</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>06</month>
<year>2016</year>
</pub-date>
<numero>54</numero>
<fpage>179</fpage>
<lpage>191</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.sa.cr/scielo.php?script=sci_arttext&amp;pid=S0256-70242016000100179&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.sa.cr/scielo.php?script=sci_abstract&amp;pid=S0256-70242016000100179&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.sa.cr/scielo.php?script=sci_pdf&amp;pid=S0256-70242016000100179&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen:En este estudio se calcula un modelo mínimo de velocidades para la Cordillera Volcánica de Guanacaste a partir de 475 sismos locales registrados por el Observatorio Vulcanológico y Sismológico Arenal Miravalles (OSIVAM) entre enero del 2006 y julio del 2014. El modelo consta de seis capas desde la superficie hasta 80 km de profundidad y posee velocidades que varían entre 3,96 y 7,79 km/s. Las correcciones para las estaciones obtenidas varían entre -0,28 a 0,45 y muestran una tendencia de valores positivos sobre el arco volcánico y negativos en el antearco, en concordancia con el espesor de la corteza. La relocalización de los sismos muestra tres grupos principales de epicentros que podrían asociarse con actividad en fallas inferidas. El MMV1D presentado en esta investigación brinda una idea simplificada de la estructura de la corteza y pretende contribuir con el mejoramiento de la localización rutinaria de sismos que realiza el OSIVAM.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract:In this study a minimum 1D model for the Guanacaste Volcanic Arc (CVG) is derived from 475 local earthquakes registered between January 2006 and July 2014 by the Arenal-Miravalles Seismological and Volcanic Observatory (OSIVAM). This velocity model has six layers and covers from the surface to a depth of 80 km. The model has velocities from 3.96 to 7.79 km/s from top to bottom. The station corrections obtained range between -0.28 and 0.45. These corrections show a trend with positive values located over the volcanic arc and negative values located on the forearc, in agreement with the crustal thickness. Three main seismicity clusters were acknowledged from the earthquake relocations, which may be associated with activity on inferred faults. The obtained one dimensional velocity model displays a simplified version for the crustal structure and aim to improve the earthquake location processes performed by the OSIVAM.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[Modelo mínimo de velocidad]]></kwd>
<kwd lng="es"><![CDATA[sismicidad de Costa Rica]]></kwd>
<kwd lng="es"><![CDATA[Cordillera Volcánica de Guanacaste]]></kwd>
<kwd lng="es"><![CDATA[Estructura de la corteza]]></kwd>
<kwd lng="es"><![CDATA[Redes sísmicas]]></kwd>
<kwd lng="en"><![CDATA[Minimum 1D velocity model]]></kwd>
<kwd lng="en"><![CDATA[seismicity of Costa Rica]]></kwd>
<kwd lng="en"><![CDATA[Guanacaste volcanic arc]]></kwd>
<kwd lng="en"><![CDATA[crust structure]]></kwd>
<kwd lng="en"><![CDATA[seismic network]]></kwd>
</kwd-group>
</article-meta>
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