<?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>0122-5383</journal-id>
<journal-title><![CDATA[CT&F - Ciencia, Tecnología y Futuro]]></journal-title>
<abbrev-journal-title><![CDATA[C.T.F Cienc. Tecnol. Futuro]]></abbrev-journal-title>
<issn>0122-5383</issn>
<publisher>
<publisher-name><![CDATA[Instituto Colombiano del Petróleo (ICP) - ECOPETROL S.A.]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S0122-53832019000200037</article-id>
<article-id pub-id-type="doi">10.29047/01225383.119</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[SUBMARINE CANYON-FILL RECONSTRUCTION FROM INTEGRATED SEISMIC-STRATIGRAPHIC ANALYSIS -APPLICATION TO BANQUEREAU FORMATION, SCOTIAN BASIN -OFFSHORE CANADA.]]></article-title>
<article-title xml:lang="es"><![CDATA[RECONSTRUCCIÓN DEL RELLENO DE UN CAÑÓN SUBMARINO A PARTIR DE ANÁLISIS SISMOESTRATIGRÁFICO INTEGRADO - APLICACIÓN A LA FORMACIÓN BANQUERAU, CUENCA ESCOCIA - COSTA AFUERA CANADÁ]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Patricia]]></surname>
<given-names><![CDATA[Chajin]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Erick J.]]></surname>
<given-names><![CDATA[Illidge]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Sait]]></surname>
<given-names><![CDATA[Khurama]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Ecopetrol - Instituto Colombiano del Petróleo Grupo de Investigación en Inversión y Modelado Geofísico IMGeo ]]></institution>
<addr-line><![CDATA[Bucaramanga ]]></addr-line>
<country>Colombia</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad Industrial de Santander  ]]></institution>
<addr-line><![CDATA[Bucaramanga ]]></addr-line>
<country>Colombia</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>12</month>
<year>2019</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>12</month>
<year>2019</year>
</pub-date>
<volume>9</volume>
<numero>2</numero>
<fpage>37</fpage>
<lpage>52</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.co/scielo.php?script=sci_arttext&amp;pid=S0122-53832019000200037&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.co/scielo.php?script=sci_abstract&amp;pid=S0122-53832019000200037&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.co/scielo.php?script=sci_pdf&amp;pid=S0122-53832019000200037&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT Building geological models (integrating stratigraphic, structural and paleo-environmental 3D models) that allow the interpretation of sand bodies deposited by turbidity currents along submarine canyons or channels, is one of the most useful tools used by geoscientists for the definition of new drilling opportunities in both exploration and development phases. In this context, the integration of methodologies such as sequence stratigraphy and seismic attributes, together with well-log and core information, outline the basis for the interpretation of sand-body lithostratigraphy and chronostratigraphy. Similarly, these models allow the interpreter to reconstruct the depositional environment and deformation history of a sedimentary basin [1]. Based on a series of chronostratigraphic stages, this paper proposes a 3D model for the sedimentation history of the Banquereau Formation. This model is based on the integration of seismic stratigraphy, seismic attribute interpretation and well-log analysis. Also, a set of system tracts and corresponding transgression and regression phases were identified for the sedimentary interval of interest. The available dataset provided the information to identify the geometry and changes in the sedimentation patterns of the stratigraphic sequences from the Tertiary to the present, thus defining a 3D model of the sedimentological and structural architecture of this interval. Last but not least, the resulting 3D stratigraphic model made possible the identification and description of an amalgamated channel complex filling a submarine canyon associated with a fluvio-deltaic setting. This sort of analysis might be used as an analog for similar reservoirs, providing key insights and vital information for decision making.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN La construcción de modelos geológicos que permitan la interpretación de cuerpos de arena depositados por corrientes de turbidez a lo largo de cañones o canales submarinos, es una de las herramientas más utilizadas por los geocientíficos para la definición de nuevas oportunidades de perforación en las fases de exploración y desarrollo. En este contexto, la integración de metodologías como estratigrafía de secuencias y atributos sísmicos, en conjunto con información de registros de pozo y de núcleos, esbozan las bases para la interpretación litoestratigráfica y cronoestratigráfica de cuerpos de arena. De la misma manera, estos modelos permiten al intérprete reconstruir el ambiente de depósito y la historia de deformación de una Cuenca sedimentaria. Basado en una serie de etapas cronoestratigráficas, este artículo propone un modelo 3D para la historia de sedimentación de la Formación Banquerau. Este modelo se basa en la integración de estratigrafía sísmica, la interpretación de atributos sísmicos y el análisis de registros de pozo. También, se identificó un conjunto de system tracts y sus correspondientes fases de transgresión y regresión para el intervalo sedimentario de interés. Los datos disponibles proporcionaron la información para identificar la geometría y los cambios en los patrones de sedimentación de las secuencias estratigráficas desde el Terciario hasta el presente, definiendo así un modelo 3D de la arquitectura sedimentológica y estructural de este intervalo. Por último, pero no menos importante, el modelo estratigráfico 3D resultante hizo posible la identificación y la descripción de un un complejo de canales amalgamados rellenando un cañón submarino asociado con un entorno fluvio-deltáico. Este tipo de análisis podría ser usado como un análogo para reservorios similares, proporcionando información clave y vital para la toma de decisiones.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[Seismic Attributes]]></kwd>
<kwd lng="en"><![CDATA[Sequence Stratigraphy]]></kwd>
<kwd lng="en"><![CDATA[Well Logs]]></kwd>
<kwd lng="en"><![CDATA[Submarine Canyon]]></kwd>
<kwd lng="es"><![CDATA[Atributos sísmicos]]></kwd>
<kwd lng="es"><![CDATA[Secuencia Estatigráfica]]></kwd>
<kwd lng="es"><![CDATA[Well Logs]]></kwd>
<kwd lng="es"><![CDATA[Cañón Submarino.]]></kwd>
</kwd-group>
</article-meta>
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