<?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>1026-8774</journal-id>
<journal-title><![CDATA[Revista mexicana de ciencias geológicas]]></journal-title>
<abbrev-journal-title><![CDATA[Rev. mex. cienc. geol]]></abbrev-journal-title>
<issn>1026-8774</issn>
<publisher>
<publisher-name><![CDATA[Universidad Nacional Autónoma de México, Instituto de Geología]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S1026-87742018000300277</article-id>
<article-id pub-id-type="doi">10.22201/cgeo.20072902e.2018.3.739</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[Analogue model of gravity driven deformation in the salt tectonics zone of northeastern Mexico]]></article-title>
<article-title xml:lang="es"><![CDATA[Modelo analógico de deformación asociada a procesos gravitacionales en la zona de tectónica salina del noreste de México]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Gracia-Marroquín]]></surname>
<given-names><![CDATA[Diego]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Cerca]]></surname>
<given-names><![CDATA[Mariano]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Carreón-Freyre]]></surname>
<given-names><![CDATA[Dora]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Barrientos-García]]></surname>
<given-names><![CDATA[Bernardino]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad Nacional Autónoma de México Centro de Geociencias ]]></institution>
<addr-line><![CDATA[Juriquilla Querétaro]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad Nacional Autónoma de México Centro de Geociencias Laboratorio de Mecánica de Geosistemas]]></institution>
<addr-line><![CDATA[Juriquilla Querétaro]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Centro de Investigaciones en Óptica A.C.  ]]></institution>
<addr-line><![CDATA[León Guanajuato]]></addr-line>
<country>Mexico</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>00</month>
<year>2018</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>00</month>
<year>2018</year>
</pub-date>
<volume>35</volume>
<numero>3</numero>
<fpage>277</fpage>
<lpage>290</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1026-87742018000300277&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1026-87742018000300277&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1026-87742018000300277&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract: In the deep seated gravity-driven deformation systems of the Gulf of Mexico contemporaneous extension and contraction of the overburden is favored by mechanical decoupling from the basement along thick salt sequences (up to 4 km). The updip extension is located inland, on the continental shelf of northeast Mexico, and is characterized by extensional listric faults and roll-overs; the downdip shortening zone is located at the deep waters and is characterized by a fold and thrust belt detached above the salt layer. Two physical experiments are used to discuss some aspects of these gravity-driven systems. The experimental setup includes a motor-driven experimental table, an inclined brittle basement (1°), a silicone layer simulating the salt sequences, and sand layers simulating the pre-kinematic Jurassic-Cretaceous strata before Laramide shortening. Deformation resulted in further tilting of the basement (3° to 4°). After the onset of deformation, thin sand layers were added at regular time intervals simulating the syntectonic sedimentation. The experiments reproduced the geometry of the deformation at the frontal ramp characterized by a seaward vergent thrust and its associated deformed region (the Perdido fold belt). The fold and thrust belt localization was favored by the change in basement inclination (a built-in slope change). Key elements interpreted in one available section of the area were reproduced in the model: a) the presence of an antithethic roll-over in the extensional zone and, b) the basinward vergence of folds and thrusts observed in the downdip shortening zone in the mexican Perdido fold belt.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen: En los sistemas de deformación asociada a procesos gravitacionales del Golfo de México, la extensión y el acortamiento contemporáneo de las secuencias de cobertura fueron provocados por el desacoplamiento mecánico entre la cobertura y el basamento a lo largo de secuencias salinas de gran espesor (hasta 4 km). La extensión se localiza en la parte continental y en la plataforma del noreste de México, y se caracteriza por fallas lístricas extensionales y estratos de crecimiento con rotación sobre las fallas; la zona de acortamiento se encuentra en las aguas profundas y se caracteriza por un cinturón de pliegues y cabalgaduras despegado por encima de las capas de sal. En este trabajo se utilizan dos experimentos físicos para discutir aspectos selectos de estos sistemas. El arreglo experimental se construyó sobre una mesa automatizada e incluye un basamento quebradizo inclinado (1°), una capa de silicona que simula las secuencias de sal y capas de arena que simulan las secuencias precinemáticas del Jurásico-Cretácico, antes del acortamiento Laramide. Se llevó a cabo un acortamiento que resultó en una mayor inclinación del basamento (3° a 4°). Durante y después de finalizar la etapa de acortamiento, se agregaron capas delgadas de arena a intervalos regulares de tiempo simulando la sedimentación sintectónica. Los experimentos reprodujeron la geometría de la deformación en la rampa frontal caracterizada por una cabalgadura con vergencia hacia el mar y su área deformada asociada (el cinturón plegado Perdido). La localización de la deformación en el cinturón de pliegues y cabalgaduras fue favorecida por el cambio en la inclinación del basamento. Dos elementos clave interpretados en una sección disponible del área de estudio fueron reproducidos en el modelo: a) la presencia de un roll-over antitético en la zona extensional y, b) la vergencia hacia la cuenca del cinturón de pliegues y la cabalgadura observados en la zona de acortamiento correspondiente a la zona mexicana del cinturón plegado Perdido.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[gravity-driven deformation systems]]></kwd>
<kwd lng="en"><![CDATA[Gulf of Mexico]]></kwd>
<kwd lng="en"><![CDATA[Perdido fold belt]]></kwd>
<kwd lng="en"><![CDATA[analogue modeling]]></kwd>
<kwd lng="es"><![CDATA[sistemas de deformación asociados a procesos gravitacionales]]></kwd>
<kwd lng="es"><![CDATA[Golfo de México]]></kwd>
<kwd lng="es"><![CDATA[cinturón plegado Perdido]]></kwd>
<kwd lng="es"><![CDATA[modelado analógico]]></kwd>
</kwd-group>
</article-meta>
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