<?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>S0122-53832022000200049</article-id>
<article-id pub-id-type="doi">10.29047/01225383.401</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[DETACHMENT LEVELS OF COLOMBIAN CARIBBEAN MUD VOLCANOES]]></article-title>
<article-title xml:lang="es"><![CDATA[NIVELES DE DESPEGUE DE VOLCANES DE LODOS DEL CARIBE COLOMBIANO]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Lopez Ramos]]></surname>
<given-names><![CDATA[Eduardo]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Gonzalez Penagos]]></surname>
<given-names><![CDATA[Felipe]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Rincón Martinez]]></surname>
<given-names><![CDATA[Daniel Andrés]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Moreno Gomez]]></surname>
<given-names><![CDATA[Nestor Raul]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Empresa Colombia de Petróleos S.A, ECOPETROL  ]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
</aff>
<aff id="Af2">
<institution><![CDATA[,Ministerio de Minas y Energía  ]]></institution>
<addr-line><![CDATA[Bogotá D.C]]></addr-line>
<country>Colombia</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>12</month>
<year>2022</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>12</month>
<year>2022</year>
</pub-date>
<volume>12</volume>
<numero>2</numero>
<fpage>49</fpage>
<lpage>77</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.co/scielo.php?script=sci_arttext&amp;pid=S0122-53832022000200049&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.co/scielo.php?script=sci_abstract&amp;pid=S0122-53832022000200049&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.co/scielo.php?script=sci_pdf&amp;pid=S0122-53832022000200049&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT Regional analysis of mud volcanoes shows the regional extension of these processes in Northern Colombia. Mud volcanoes are active systems with the characteristics of the underlying sedimentary sequences on the surface, as well as the presence of hydrocarbons. These provide information about the oil systems and the characterization of new migration paths. New data acquired during field geology studies, along with the evaluation of acquired aerial images by dron, allowed observation of variations in terms of morphology and neotectonic process, being distinctive among mud volcanoes formed on different structural domains. Mud volcanoes formed in basement areas without thrust faults (Hangingwall realm of the San Jacinto Fault) are usually circular, connected to the basement by regional faults. Other mud volcanoes formed in older and younger deformed belts (Footwall realm of the Sinú Fault and Footwall realm of the San Jacinto Fault respectively) tend to have ellipsoidal shapes, with drainage patterns that suggest local stress fields associated with regional strike-slip movements of major faults. The analysis of U/Pb ages in detrital zircons extracted from mud volcanoes and outcropping sedimentary sequences in the Colombian Caribbean, together with the analysis of foraminifera and palynomorphs, suggest different levels of detachment. Clay mineralogy and geochemistry indicate that mud volcanoes formed in the backstop and the Northern part of the San Jacinto deformed belt have sludge material from sedimentary sequences, with contribution from continental basement rocks, while the mud volcanoes in the central and Southern parts of the studied area tend to show sediments from deepest stratigraphic levels, derived from less evolved magmatic sources (dioritic basements). Gas and water analyses from studied mud volcanoes suggest that the old deformed belt, Paleocene accretionary wedge, and backstop areas, have evidence of thermogenic oil systems, while in the younger deformed belt domain, the tendency is to suggest microbial processes.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN El análisis regional de los volcanes de lodo muestra la extensión regional del fenómeno en el norte de Colombia. Los volcanes de lodo son sistemas activos que manifiestan las características de las secuencias sedimentarias subyacentes en la superficie, así como la presencia de hidrocarburos, lo que brinda información sobre los sistemas petroleros y la caracterización de nuevas rutas migratorias. Los nuevos datos adquiridos durante los trabajos de geología de campo, junto con la adquisición de imágenes aéreas por dron, permitieron observar variaciones en términos de morfología y procesos neotectónicos, siendo distintivos entre volcanes de lodo formados en diferentes dominios estructurales. Así, los volcanes de lodo formados en áreas de basamento no afectado por fallas inversas (Dominio del bloque colgante de la Falla de San Jacinto) suelen ser circulares, conectados al basamento por fallas regionales, mientras que los volcanes formados en cinturones deformados viejos y jóvenes (dominios de los bloques yacentes de las fallas de Sinú y San Jacinto respectivamente), tienden a presentar formas elipsoidales, con patrones de drenajes que sugieren campos de tensión local asociados a movimientos fallas rumbodeslizantes mayores. El análisis de edades U/Pb en circones detríticos extraidos de los volcanes de lodo y secuencias sedimentarias aflorantes en el Caribe Colombiano, sumado al análisis de faunas de foraminíferos y palinomorfos, sugieren niveles de despegue diversos. Los análisis de mineralogía y geoquímica de arcilla indican que los volcanes de lodo formados en el contrafuerte rígido y la parte norte del cinturón deformado de San Jacinto, tienen lodos originados en secuencias sedimentarias, con aportes de rocas de basamento continental, mientras que los volcanes de lodo ubicados en las partes central y sur de el área estudiada, tienden a mostrar lodos provistos desde niveles estratigráficos profundos derivados de fuentes ígneas menos evolucionadas (basamentos dioríticos). Los análisis de gas y agua obtenidos de varios volcanes de lodo sugieren que el antiguo cinturón deformado, la cuña de acreción del Paleoceno y las áreas de contrafuerte rígido, tienen evidencias de sistemas de petróleo termogénico, mientras que, en el dominio del cinturón deformado más joven, la tendencia es a mostrar evidencias de sistemas microbianos.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[Mud volcanoes]]></kwd>
<kwd lng="en"><![CDATA[Geochemistry]]></kwd>
<kwd lng="en"><![CDATA[Northern Colombia]]></kwd>
<kwd lng="en"><![CDATA[Petroleum systems]]></kwd>
<kwd lng="es"><![CDATA[Volcanes de lodo]]></kwd>
<kwd lng="es"><![CDATA[Norte de Colombia]]></kwd>
<kwd lng="es"><![CDATA[Geoquímica]]></kwd>
<kwd lng="es"><![CDATA[Sistemas petrolíferos]]></kwd>
</kwd-group>
</article-meta>
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