<?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>0120-0283</journal-id>
<journal-title><![CDATA[Boletín de Geología]]></journal-title>
<abbrev-journal-title><![CDATA[Bol. geol.]]></abbrev-journal-title>
<issn>0120-0283</issn>
<publisher>
<publisher-name><![CDATA[Universidad Industrial de Santander]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S0120-02832021000200095</article-id>
<article-id pub-id-type="doi">10.18273/revbol.v43n2-2021006</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[Geochemistry and petrographic analysis of Los Cuervos and Molino formations, Cesar Sub-Basin (Colombia): Implications in the petroleum system evolution]]></article-title>
<article-title xml:lang="es"><![CDATA[Análisis geoquímico y petrográfico de las formaciones Los Cuervos y Molino, Subcuenca Cesar (Colombia): implicaciones en la evolución del sistema petrolero]]></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"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[García-González]]></surname>
<given-names><![CDATA[Mario]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</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"/>
</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"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,aff1  ]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
<country>Colombia</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,aff2  ]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
<country>Colombia</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>08</month>
<year>2021</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>08</month>
<year>2021</year>
</pub-date>
<volume>43</volume>
<numero>2</numero>
<fpage>95</fpage>
<lpage>116</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.co/scielo.php?script=sci_arttext&amp;pid=S0120-02832021000200095&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.co/scielo.php?script=sci_abstract&amp;pid=S0120-02832021000200095&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.co/scielo.php?script=sci_pdf&amp;pid=S0120-02832021000200095&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract A geochemical characterization of Los Cuervos and Molino formations in the Cesar Sub-Basin was carried out using core samples obtained from the ANH-La Loma-1 Well. A total of 113 Rock-Eval pyrolysis analysis, total organic carbon (TOC), total sulphur content (TS) analysis, 13 vitrinite reflectance analysis (%Ro) and 30 thin-section petrographic analysis were performed. Based on these new data, it was possible to classify the quality of organic matter and the current thermal maturation of Los Cuervos and Molino formations. Additionally, a petrographic characterization of 30 samples allowed the correlation of the lithology with the geochemical results. Also, one-dimensional geochemical modelling was implemented in order to contribute to the knowledge of the evolution of the oil system in the Cesar Sub-Basin. The spatial distribution of the formations used in the modelling was obtained from 2 seismic lines two-way time. The results obtained indicate that Los Cuervos Formation presents TOC values from 0.29 to 66.55%, TS values from 0.02 to 11.29%, their organic matter consisted of type III kerogen which is consistent with an immature thermal maturation stage. In contrast, the Molino Formation presents TOC values from 0.23 to 2.28%, TS values from 0.001 to 1.39%, their organic matter consisted of type II/III kerogen this suggests an early entry to the oil window with a maximum pyrolysis temperature (Tmax) value of 442°C. The geochemical modelling tunes better with measured data from palaeo-geothermometers (%Ro and Tmax). The geochemical modelling shows that, between 60 - 40 million years ago (mya), the Cretaceous formations entered in the oil generation window and it is expected that, between 40 - 30 mya, the Lagunitas, Aguas Blancas, and La Luna formations will be at their peak of hydrocarbon generation.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen Las muestras de núcleo obtenidas del Pozo ANH-La Loma-1 localizado en la Subcuenca Cesar permitieron la caracterización geoquímica de las formaciones Los Cuervos y Molino. Se realizaron un total de 113 análisis de pirólisis Rock-Eval, de carbono orgánico total (COT) y de contenido de azufre total (TS), 13 análisis de reflectancia de vitrinita (%Ro) y 30 análisis petrográficos de secciones delgadas. Basados en estos nuevos datos se pudo establecer la calidad de la materia orgánica y la condición actual de la maduración termal de las formaciones. Adicionalmente, la caracterización petrográfica de 30 muestras permitió la correlación de la litología con los resultados geoquímicos. También, se realizó un modelamiento geoquímico 1D con la finalidad de aportar en el conocimiento de la evolución del sistema petrolífero de la Subcuenca Cesar. La distribución espacial de las formaciones usada en el modelamiento fue obtenida de 2 líneas sísmicas 2D en tiempo. Los resultados obtenidos indican que la Formación Los Cuervos presenta valores de COT de 0,29-66,55%, valores de TS de 0,02-11,29%, su materia orgánica es de kerógeno tipo III el cual es consistente con un estado de madurez termal inmaduro. En contraste, la Formación Molino presenta valores de COT de 0,23-2,28%, valores de TS de 0,001-1,39%, su materia orgánica es de kerógeno tipo II/III, esto sugiere una temprana entrada en ventana de generación con un valor de Tmáx de 442°C. El modelo geoquímico calibra bien con los datos medidos de paleo-geotermómetros (%Ro y Tmáx) y muestra que entre 60 - 40 Ma las formaciones Cretácicas entraron en ventana de generación de hidrocarburos y se espera que entre 40-30 Ma las formaciones Lagunitas, Aguas Blancas y La Luna se encuentren en su pico de generación de hidrocarburos.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[Los Cuervos Formation]]></kwd>
<kwd lng="en"><![CDATA[Molino Formation]]></kwd>
<kwd lng="en"><![CDATA[Geochemical modelling]]></kwd>
<kwd lng="en"><![CDATA[Source rock]]></kwd>
<kwd lng="en"><![CDATA[Cesar Sub-Basin]]></kwd>
<kwd lng="en"><![CDATA[Cesar Ranchería Basin.]]></kwd>
<kwd lng="es"><![CDATA[Formación Los Cuervos]]></kwd>
<kwd lng="es"><![CDATA[Formación Molino]]></kwd>
<kwd lng="es"><![CDATA[Modelamiento geoquímico]]></kwd>
<kwd lng="es"><![CDATA[Roca fuente]]></kwd>
<kwd lng="es"><![CDATA[Subcuenca Cesar]]></kwd>
<kwd lng="es"><![CDATA[Cuenca Cesar Ranchería.]]></kwd>
</kwd-group>
</article-meta>
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