<?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>S0120-02832023000300095</article-id>
<article-id pub-id-type="doi">10.18273/revbol.v45n3-2023006</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Modelo del entrampamiento de hidrocarburos mio-plioceno del Bloque Oritupano-Leona (Subcuenca de Maturín, Cuenca Oriental de Venezuela): una revisión]]></article-title>
<article-title xml:lang="en"><![CDATA[The Mio-Pliocene model for hydrocarbon entrapment of the Oritupano-Leona Block (Maturín Sub-Basin, Eastern Basin of Venezuela): a review]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Rossello]]></surname>
<given-names><![CDATA[Eduardo A.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Ldpez-Gamundi]]></surname>
<given-names><![CDATA[Oscar R.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Mozetic]]></surname>
<given-names><![CDATA[Marcos E.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad de Buenos Aires Departamento de Ciencias Geológicas ]]></institution>
<addr-line><![CDATA[Buenos Aires ]]></addr-line>
<country>Argentina</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,P1Consultants  ]]></institution>
<addr-line><![CDATA[Houston ]]></addr-line>
<country>USA</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Consultor independiente  ]]></institution>
<addr-line><![CDATA[Madrid ]]></addr-line>
<country>España</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>12</month>
<year>2023</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>12</month>
<year>2023</year>
</pub-date>
<volume>45</volume>
<numero>3</numero>
<fpage>95</fpage>
<lpage>118</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.co/scielo.php?script=sci_arttext&amp;pid=S0120-02832023000300095&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.co/scielo.php?script=sci_abstract&amp;pid=S0120-02832023000300095&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.co/scielo.php?script=sci_pdf&amp;pid=S0120-02832023000300095&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen El Bloque Oritupano-Leona (BOL) está localizado en la prolífera Subcuenca de Maturín perteneciente a la Cuenca Oriental de Venezuela en el flanco sur de la plataforma de antepaís cercana al Río Orinoco. A partir de la interpretación sísmica disponible, se reconoce un modelo estructural 3D relacionado sintectónicamente con la secuencia del Mioceno Inferior-Plioceno a partir de tres sistemas de fallas de crecimiento formadas por segmentos subordinados en el Mioceno Inferior (17,3 Ma), Mioceno Medio (15,35 Ma) y Mioceno Superior-Plioceno. El estilo estructural exhibe fallas normales de rumbo E-O inclinadas al Norte (fallamiento sintético) o al Sur en contrapendiente regional (fallamiento antitético) conformando pilares tectónicos y pliegues de arrastre asociados afectados por fallas transpresivas dextrales de rumbo NE-SO inclinadas al NO con extremos solapados por propagación lateral y vertical. Los fallamientos generan ambientes propicios para el acomodamiento de volúmenes sinsedimentarios con potencias variables entre los tramos intermedios y centrales de los segmentos de fallas que contienen los principales entrampamientos de los niveles de las formaciones Oficina y Merecure, responsables de los recursos hidrocarburíferos del BOL. Las morfologías estructurales se vinculan con un escenario transtensivo dextral relacionado con un levantamiento flexural durante los tiempos Oligoceno-Mioceno por la traslación oriental de la placa Caribe a lo largo del límite septentrional de la placa Sudamérica. El presente análisis aporta criterios estructurales que contribuyen con la definición de estrategias para la exploración y desarrollo de objetivos exploratorios remanentes.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract The Oritupano-Leona Block (BOL) is located along the southern margin of the prolific Maturín Sub-Basin (Eastern Basin of Venezuela). From the available seismic interpretation, a 3D structural model for the Lower Miocene-Pliocene sequence is proposed based on three growth fault systems formed by subordinate segments in the Lower Miocene (17.3 Ma), Middle Miocene (15.35 Ma), and Late Miocene-Pliocene. The structural style is characterized by E-W synthetic normal faults dipping to the North or to the South in a regional counterslope (antithetic faulting) forming tectonic pillars and associated drag folds affected by NE-SW oriented, dextral transpressive faults dipping to the NW with overlapping ends due to lateral and vertical propagation. The faults generated the accommodation for growth strata synsedimentary-with variable strengths between the intermediate and central sections of the fault segments, where traps were formed for the sandstones of the Oficina and Merecure formations. The structural morphologies are linked to a dextral transtensive system related to a flexural uplift during Oligocene-Miocene times due to the eastern translation of the Caribbean plate along the northern limit of the South American plate. This analysis provides structural criteria that contribute to the definition of strategies for exploration and development of remaining exploratory targets.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[Fallas de crecimiento]]></kwd>
<kwd lng="es"><![CDATA[Pliegues de arrastre]]></kwd>
<kwd lng="es"><![CDATA[Transcurrencia]]></kwd>
<kwd lng="es"><![CDATA[Trampas de hidrocarburos]]></kwd>
<kwd lng="es"><![CDATA[Tectosedimentación]]></kwd>
<kwd lng="en"><![CDATA[Growth faults]]></kwd>
<kwd lng="en"><![CDATA[Drag folds]]></kwd>
<kwd lng="en"><![CDATA[Transcurrent system]]></kwd>
<kwd lng="en"><![CDATA[Hydrocarbon traps]]></kwd>
<kwd lng="en"><![CDATA[Tectosedimentation]]></kwd>
</kwd-group>
</article-meta>
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