<?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>S0256-70242021000200020</article-id>
<article-id pub-id-type="doi">10.15517/rgac.v0i65.46700</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Estratigrafía sedimentaria Cretácico-Paleógeno de la cuenca de Limón Sur, Costa Rica]]></article-title>
<article-title xml:lang="en"><![CDATA[Cretaceous-Paleogene sedimentary stratigraphy, Limon Sur Basin, Costa Rica]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Aguilar]]></surname>
<given-names><![CDATA[Teresita]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Denyer]]></surname>
<given-names><![CDATA[Percy]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad de Costa Rica (UCR) Centro de Investigación en Ciencias Geológicas (CICG) ]]></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>20</fpage>
<lpage>43</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.sa.cr/scielo.php?script=sci_arttext&amp;pid=S0256-70242021000200020&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.sa.cr/scielo.php?script=sci_abstract&amp;pid=S0256-70242021000200020&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.sa.cr/scielo.php?script=sci_pdf&amp;pid=S0256-70242021000200020&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen La cuenca Limón Sur ha sido relativamente bien estudiada, por su importancia económica, sus dimensiones y características especiales. Sin embargo, todavía quedan muchos aspectos por investigar para definir la estratigrafía y la evolución tectónica de la región. En este trabajo se sintetizan los estudios que se han podido recopilar, que abarcan el Cretácico y Paleógeno, quedando el Neógeno para futuras publicaciones. La secuencia de más de 6000 m inicia con rocas de origen marino profundo, Formación Changuinola, del Cretácico Superior, aún no identificada en el territorio costarricense, seguida por la Formación Río Lari del ¿Cretácico? - Paleoceno, también formada en un ambiente marino de talud o más profundo. La Formación Tuis del Eoceno Superior-Oligoceno Inferior se formó en un ambiente de talud, conformando depósitos turbidíticos. A partir de este punto se depositaron unidades calcáreas en un ambiente nerítico, como las calizas de la Formación Fila de Cal del Eoceno, las calcilutitas y limolitas de la Formación Senosri y las calizas de la Formación Punta Pelada del Oligoceno. Esta secuencia está cubierta por lutitas, areniscas y conglomerados de las formaciones más jóvenes del Mioceno y Plioceno, como Uscari, Río Banano, Limón y Suretka.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract The Limón Sur basin has been relatively well studied given its economic importance, its dimensions and special characteristics. However, further research is required to determine the stratigraphy and tectonic evolution of this region. This work summarizes available studies covering the Cretaceous and Paleogene, excluding Neogene for future publications. The sequence of over 6,000 m begins with rocks originated in a deep marine environment -the Changuinola Formation- of late Cretaceous age which has not yet been identified in Costa Rican territory, followed by the Río Lari Formation Cretaceous? - Paleocene, also formed in a slope marine environment or deeper. The Tuis Formation of the Upper Eocene-Lower Oligocene corresponds with turbidite deposits formed in a marine slope environment. From this point, limestone units were deposited in a neritic environment, such as the limestones of the Eocene Fila de Cal Formation, the calcilutites and siltstones of Senosri Formation and the limestones of the Punta Pelada Formation of Oligocene age. This sequence is covered by lutites, sandstones and conglomerates from the younger Miocene and Pliocene formations, such as Uscari, Río Banano, Limón and Suretka.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[Cretaceous-Paleogene]]></kwd>
<kwd lng="en"><![CDATA[Geologic Section]]></kwd>
<kwd lng="en"><![CDATA[Southeast of Costa Rica]]></kwd>
<kwd lng="en"><![CDATA[Petroleum]]></kwd>
<kwd lng="en"><![CDATA[Stratigraph]]></kwd>
<kwd lng="en"><![CDATA[Northwest of Panama.]]></kwd>
<kwd lng="es"><![CDATA[Cretácico-Paleógeno]]></kwd>
<kwd lng="es"><![CDATA[sección geológica]]></kwd>
<kwd lng="es"><![CDATA[sureste de Costa Rica]]></kwd>
<kwd lng="es"><![CDATA[petróleo]]></kwd>
<kwd lng="es"><![CDATA[estratigrafía]]></kwd>
<kwd lng="es"><![CDATA[noroeste de Panamá.]]></kwd>
</kwd-group>
</article-meta>
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