<?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>S0256-70242021000200321</article-id>
<article-id pub-id-type="doi">10.15517/rgac.v0i65.46876</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[El altiplano de Grano de Oro (Moravia, Chirripó): una cuenca reciente de represamiento tectónico en Alta Talamanca, Costa Rica]]></article-title>
<article-title xml:lang="en"><![CDATA[The Grano de Oro plateau (Moravia, Chirripó): a tectonic damming basin in Alta Talamanca, Costa Rica]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Calvo]]></surname>
<given-names><![CDATA[Cristian]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Salazar]]></surname>
<given-names><![CDATA[Mónica]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Alfaro]]></surname>
<given-names><![CDATA[David]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Fregni]]></surname>
<given-names><![CDATA[Sebastián]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Alvarado]]></surname>
<given-names><![CDATA[Guillermo E.]]></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[ ]]></addr-line>
<country>Costa Rica</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Comisión Nacional de Prevención de Riesgos 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>321</fpage>
<lpage>346</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.sa.cr/scielo.php?script=sci_arttext&amp;pid=S0256-70242021000200321&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.sa.cr/scielo.php?script=sci_abstract&amp;pid=S0256-70242021000200321&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.sa.cr/scielo.php?script=sci_pdf&amp;pid=S0256-70242021000200321&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen El altiplano de Grano de Oro posee una altitud media de 1100 m s.n.m. y un área de &#8275;5.5 km2, es una anomalía morfológica en la cordillera de Talamanca, con características morfoestructurales y de sedimentología fluvial particulares. Consiste en una cuenca exorreica en la cual predomina una llanura de inundación con geoformas y litofacies típicas. Sus depósitos están distribuidos principalmente a lo largo del eje fluvial del río Moravia y dentro de las geoformas del sistema fluvial meándrico se reconocen: terrazas, barras de arena, canales, lagos, entre otros. Se propone un modelo de génesis para la cuenca en donde la geometría y cinemática de la falla Alcantarilla, al NW del altiplano, provocan un régimen transpresivo y una estructura en flor positiva, basculando el bloque estructural al E del altiplano, represando el río Moravia. La falla Alcantarilla es probablemente neotectónica, debido a la presencia de sismicidad y la edad de los depósitos en la cuenca. Las geoformas y los sedimentos observados son jóvenes y presentan una evolución elevada y variable debido al modelado permanente del paisaje posglaciar (desde el Groenlandiense) relacionado directamente con una tectónica activa leve y con alteraciones procedentes de la intervención humana, que influyen en la dinámica fluvial en el territorio.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract The Grano de Oro plateau has an average altitude of 1,100 m a.s.l. and an area of &#8275;5.5 km2, it is a morphological anomaly in the Talamanca mountain range, with particular morphostructural and fluvial sedimentology characteristics. It consists of an exorheic basin in which a floodplain predominates with typical geoforms and lithofacies. Its deposits are mainly distributed along the fluvial axis of the Moravia River and within the geoforms of the meandering fluvial system are recognized: terraces, sand bars, channels, lakes, among others. A genesis model is proposed for the basin where the geometry and kinematics of the Alcantarilla fault, to the NW of the plateau, cause a transpressive regime and a positive flower structure, tilting the structural block to the E of the altiplano, damming the Moravia River. The Alcantarilla fault is probably neotectonic, due to the presence of seismicity and the age of the deposits in the basin. The geoforms and sediments observed are young and present a high and variable evolution due to the permanent modeling of the postglacial landscape (since the Greenlandian) directly related to mild active tectonics and alterations from human intervention, which influence the fluvial dynamics in the territory.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[Tectonic Basin]]></kwd>
<kwd lng="en"><![CDATA[Morphotectonic]]></kwd>
<kwd lng="en"><![CDATA[Tectonic Pop-Up]]></kwd>
<kwd lng="en"><![CDATA[Radiocarbon]]></kwd>
<kwd lng="en"><![CDATA[Fluvial Geomorphology]]></kwd>
<kwd lng="en"><![CDATA[Greenlandian]]></kwd>
<kwd lng="en"><![CDATA[Alcantarilla Fault]]></kwd>
<kwd lng="en"><![CDATA[Moravia River]]></kwd>
<kwd lng="es"><![CDATA[cuenca tectónica]]></kwd>
<kwd lng="es"><![CDATA[morfotectónica]]></kwd>
<kwd lng="es"><![CDATA[flor tectónica positiva]]></kwd>
<kwd lng="es"><![CDATA[radiocarbono]]></kwd>
<kwd lng="es"><![CDATA[geomorfología fluvial]]></kwd>
<kwd lng="es"><![CDATA[Groenlandiense]]></kwd>
<kwd lng="es"><![CDATA[falla Alcantarilla]]></kwd>
<kwd lng="es"><![CDATA[río Moravia]]></kwd>
</kwd-group>
</article-meta>
</front><back>
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