<?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>1794-6190</journal-id>
<journal-title><![CDATA[Earth Sciences Research Journal]]></journal-title>
<abbrev-journal-title><![CDATA[Earth Sci. Res. J.]]></abbrev-journal-title>
<issn>1794-6190</issn>
<publisher>
<publisher-name><![CDATA[Universidad Nacional de Colombia]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S1794-61902021000200179</article-id>
<article-id pub-id-type="doi">10.15446/esrj.v25n2.86025</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[Thermal evolution of Los Cuervos formation in the southern area of the Cesar sub-basin (Colombia), based on geochemical and petrophysical data]]></article-title>
<article-title xml:lang="es"><![CDATA[Evolución termal de la formación Los Cuervos, en el área sur de la subcuenca Cesar, con base en datos geoquímicos y petrofísicos]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Avendaño-Sánchez]]></surname>
<given-names><![CDATA[Gladys Marcela]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
<xref ref-type="aff" rid="Aaf"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[García-González]]></surname>
<given-names><![CDATA[Mario]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
<xref ref-type="aff" rid="Aaf"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Cruz-Guevara]]></surname>
<given-names><![CDATA[Luis Enrique]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
<xref ref-type="aff" rid="Aaf"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Cruz-Ceballos]]></surname>
<given-names><![CDATA[Luis Felipe]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
<xref ref-type="aff" rid="Aaf"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad Industrial de Santander  ]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
<country>Colombia</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Grupo de Investigación en Geología Básica y Aplicada (GIGBA)  ]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
<country>Colombia</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Energy and Other Non-Renewable Resources Research Group  ]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>06</month>
<year>2021</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>06</month>
<year>2021</year>
</pub-date>
<volume>25</volume>
<numero>2</numero>
<fpage>179</fpage>
<lpage>192</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.co/scielo.php?script=sci_arttext&amp;pid=S1794-61902021000200179&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.co/scielo.php?script=sci_abstract&amp;pid=S1794-61902021000200179&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.co/scielo.php?script=sci_pdf&amp;pid=S1794-61902021000200179&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT The tectonic complexity that occurred during the Cenozoic at the Cesar-Ranchería Basin (Colombia) has generated changes in the evolution of its petroleum system. Proof of this is the lack of stratigraphic records in the Cesar sub-basin during both the early Eocene and in the late Eocene-early Miocene interval. In this study, authors analyzed information already published regarding the sub-basin and new geochemical data obtained from Rock-Eval pyrolysis analyses and vitrinite reflectance (Ro%). The core samples used are from the ANH-La Loma-2 and ANH-CR-Los Cerezos-1X wells. Based on this information, Los Cuervos Formation was classified as a source rock for its geochemical characteristics. Additionally, the geochemical and petrophysical results indicate continuous deposition of sediments from the Paleocene to the late Eocene. These results were obtained using samples from two wells (Calenturitas and La Jagua) at Los Cuervos Formation and the paleo-geothermometer data of Paleocene formations. Based on density and compaction conditions, it is clear that it corresponds to a sequence of quartz sandstones. Therefore, it is expected the Eocene Sedimentites unit has reached a thickness between 2.5 to 3.5 km. According to recent thermo-chronological studies, this unit began to be eroded from the late Eocene to the early Miocene. The evidence obtained helped improve the knowledge in the thermal evolution model of the petroleum system, establish the time when the organic transformation ratios (TR) occurred, and estimate the current state of the Cretaceous source rocks of the Cesar sub-basin.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN La complejidad tectónica a la cual fue sometida la cuenca Cesar-Ranchería durante el Cenozoico generó cambios en la evolución de su sistema petrolífero. Prueba de ello es la falta de registro estratigráfico en la subcuenca Cesar durante el Eoceno temprano y el intervalo Eoceno-Mioceno temprano. En este estudio los autores analizan la información publicada y nuevos datos de pirolisis Rock-Eval y de reflectancia de vitrinita (Ro%) con muestras de núcleos de perforación de dos nuevos pozos (ANH-La Loma-2 y ANH-CR-Los Cerezos-1X). Basados en esta información fue posible clarificar las características geoquímicas de la Formación Los Cuervos como roca fuente de hidrocarburos. Adicionalmente, los resultados geoquímicos y petrofísicos, obtenidos con muestras de dos pozos (Calenturitas y La Jagua) de la Formación Los Cuervos y datos de paleogeotermómetros de formaciones del Paleoceno, indicaron la existencia de una depositación continua de sedimentos desde el Paleoceno hasta el Eoceno tardío. Con base en las condiciones de densidad y compactación observadas es claro que esto corresponde a una secuencia de areniscas de cuarzo. Por lo tanto, se espera que la unidad de sedimentitas del Eoceno haya alcanzado un espesor de 2.5 - 3.5 km. Esta unidad de roca, de acuerdo con estudios recientes de termocronología, comenzó a ser erosionada en el Eoceno tardío y hasta el Mioceno temprano. La evidencia obtenida permitió mejorar el modelo de evolución termal del sistema petrolífero, establecer el tiempo en el cual ocurrieron las transformaciones orgánicas y estimar cómo están actualmente las rocas generadoras del Cretáceo de la subcuenca Cesar.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[Cesar-Rancheria Basin]]></kwd>
<kwd lng="en"><![CDATA[Cesar sub-basin]]></kwd>
<kwd lng="en"><![CDATA[Los Cuervos Formation]]></kwd>
<kwd lng="en"><![CDATA[Source Rock]]></kwd>
<kwd lng="en"><![CDATA[Geochemical Modelling]]></kwd>
<kwd lng="en"><![CDATA[Porosity-Depth Relation]]></kwd>
<kwd lng="es"><![CDATA[Algoritmo de localización 3D]]></kwd>
<kwd lng="es"><![CDATA[interferencia masiva y no masiva]]></kwd>
<kwd lng="es"><![CDATA[geoestratigrafía]]></kwd>
<kwd lng="es"><![CDATA[roca circundante]]></kwd>
<kwd lng="es"><![CDATA[REE]]></kwd>
<kwd lng="es"><![CDATA[rastro]]></kwd>
</kwd-group>
</article-meta>
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