<?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>0370-3908</journal-id>
<journal-title><![CDATA[Revista de la Academia Colombiana de Ciencias Exactas, Físicas y Naturales]]></journal-title>
<abbrev-journal-title><![CDATA[Rev. acad. colomb. cienc. exact. fis. nat.]]></abbrev-journal-title>
<issn>0370-3908</issn>
<publisher>
<publisher-name><![CDATA[Academia Colombiana de Ciencias Exactas, Físicas y Naturales]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S0370-39082018000400402</article-id>
<article-id pub-id-type="doi">10.18257/raccefyn.673</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Modelo estructural del Campo Escuela Colorado a partir de modelos análogos]]></article-title>
<article-title xml:lang="en"><![CDATA[Structural model of Campo Escuela Colorado based on analog models]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Anaya]]></surname>
<given-names><![CDATA[Camilo]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Jiménez-Díaz]]></surname>
<given-names><![CDATA[Giovanny]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Martínez-Sánchez]]></surname>
<given-names><![CDATA[Dilan A.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad Industrial de Santander Escuela de Geología ]]></institution>
<addr-line><![CDATA[Bucaramanga ]]></addr-line>
<country>Colombia</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad Industrial de Santander Escuela de Geología Grupo de Investigación en Geología Básica y Aplicada (GIGBA)]]></institution>
<addr-line><![CDATA[Bucaramanga ]]></addr-line>
<country>Colombia</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>12</month>
<year>2018</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>12</month>
<year>2018</year>
</pub-date>
<volume>42</volume>
<numero>165</numero>
<fpage>402</fpage>
<lpage>409</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.co/scielo.php?script=sci_arttext&amp;pid=S0370-39082018000400402&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.co/scielo.php?script=sci_abstract&amp;pid=S0370-39082018000400402&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.co/scielo.php?script=sci_pdf&amp;pid=S0370-39082018000400402&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen La cuenca del Valle Medio del Magdalena es una cuenca intermontana (Cooper, et al., 1995; Taboada, et al., 2000; Sarmiento-Rojas, et al., 2006), que se caracteriza por tener estructuras con doble vergencia y está limitada por las cordilleras Central y Oriental (Córdoba, et al., 2000). En el sector sureste del Valle, asociado al frente de deformación occidental de la Cordillera Oriental, se localiza el Campo Escuela Colorado de la Universidad Industrial de Santander. Los estudios previos (Ecopetrol, 2003; Chajín, et al., 2013; Zafra, 2013) en dicho campo difieren en cuanto al modelo estructural y su relación con las estructuras regionales (por ejemplo, la falla de La Salina). En este trabajo se presentan los resultados de 15 modelos de simulación de una cuña crítica para definir las características estructurales en un ambiente compresivo. Los resultados de los modelos muestran un frente de deformación dominado por fallas con vergencia hacia el promontorio y retrocabalgamientos asociados. El apilamiento de material causó elevación topográfica en la zona axial de la cuña. Con base en la tendencia observada en los 15 experimentos realizados, se concluyó que la geometría de las estructuras está dominada por la escamación delgada y que el modelo estructural que define al Campo Escuela Colorado es una zona triangular controlada por un retrocabalgamiento.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract The Middle Magdalena Valley is an intermontane basin (Cooper, et al., 1995; Taboada, et al., 2000; Sarmiento- Rojas, et al., 2006) characterized by double vergence structures and flanked by the Central and Eastern Cordilleras (Córdoba, et al., 2000). The Campo Escuela Colorado oil field of the Universidad Industrial de Santander is located in the South Eastern zone of the Valley, associated with the western deformation front of the Eastern Cordillera. Previous works on this oil field have diverged as regards the structural model and the relationship with major structures (e.g., La Salina Fault). We present the results of 15 critical wedge simulation models to define the main structural characteristics in a compressive tectonic setting. Our results showed a deformation front dominated by thrust faults that verge towards the foreland and by associated backthrusts. The topographic elevation is caused by material stacked in the axial zone of the wedge. Based on the 15 experimental models we concluded that the geometry of the structure is dominated by thin flaking and that the structural model of the Campo Escuela Colorado is a triangular zone dominated by a backthrust.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[Estilo estructural]]></kwd>
<kwd lng="es"><![CDATA[Valle Medio del Magdalena]]></kwd>
<kwd lng="es"><![CDATA[Campo Escuela Colorado]]></kwd>
<kwd lng="es"><![CDATA[Modelos análogos]]></kwd>
<kwd lng="en"><![CDATA[Structural style]]></kwd>
<kwd lng="en"><![CDATA[Middle Magdalena Valley]]></kwd>
<kwd lng="en"><![CDATA[Campo Escuela Colorado]]></kwd>
<kwd lng="en"><![CDATA[Analog models]]></kwd>
</kwd-group>
</article-meta>
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