<?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>1405-3322</journal-id>
<journal-title><![CDATA[Boletín de la Sociedad Geológica Mexicana]]></journal-title>
<abbrev-journal-title><![CDATA[Bol. Soc. Geol. Mex]]></abbrev-journal-title>
<issn>1405-3322</issn>
<publisher>
<publisher-name><![CDATA[Sociedad Geológica Mexicana A.C.]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S1405-33222023000300107</article-id>
<article-id pub-id-type="doi">10.18268/bsgm2023v75n3a070623</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Modelamiento análogo de la tectónica salina asociada a ambientes compresivos y zonas transversales en la zona axial de la Cordillera Oriental, Colombia]]></article-title>
<article-title xml:lang="en"><![CDATA[Analogue modeling of salt tectonics associated to compressive environments and transverse zones in the axial zone of the Cordillera Oriental, Colombia]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Escalante Cárdenas]]></surname>
<given-names><![CDATA[Carlos Andrés]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Martinez-Sánchez]]></surname>
<given-names><![CDATA[Dilan Arturo]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Jiménez]]></surname>
<given-names><![CDATA[Giovanny]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad de Oulu Escuela de Minas ]]></institution>
<addr-line><![CDATA[Oulu ]]></addr-line>
<country>Finlandia</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad Industrial de Santander Escuela de Geología Grupo de Investigación en Geofísica y Geología Aplicada]]></institution>
<addr-line><![CDATA[Bucaramanga ]]></addr-line>
<country>Colombia</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Universidad Industrial de Santander Escuela de Geología Grupo de Investigación en Geología Básica y Aplicada]]></institution>
<addr-line><![CDATA[Bucaramanga ]]></addr-line>
<country>Colombia</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>00</month>
<year>2023</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>00</month>
<year>2023</year>
</pub-date>
<volume>75</volume>
<numero>3</numero>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1405-33222023000300107&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1405-33222023000300107&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1405-33222023000300107&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN Las secuencias sedimentarias con niveles evaporíticos presentan estructuras tridimensionales complejas debido a movimientos halocinéticos (tectónica salina). En el Anticlinal de Zipaquirá, ubicado en la Cordillera Oriental de Colombia, se reportan niveles salinos en las unidades del Cretácico Temprano. Este trabajo analizó estructuralmente el Anticlinal de Zipaquirá, basado en modelos análogos que simulan la relación entre la tectónica salina y las zonas trasversales que limitan y segmentan esta estructura. Los modelos se realizaron en una mesa de deformación tipo seducción con velocidad constante de desplazamiento. Los mismos simulan anisotropías de basamento mediante un bloque rígido de madera constituido por dos rampas frontales de 30° de inclinación conectadas por una rampa lateral. Adyacente, se dispone una capa de fluido no-newtoniano y capas de arena cuarzosa fina de color variable. Se efectuaron tres configuraciones con diferentes distribuciones de la capa de fluido no-newtoniano: A) continua delgada, B) discontinua y C) continua espesa. Para cada configuración se llevaron a cabo al menos 15 experimentos. Los resultados del modelamiento análogo mostraron un cuerpo salino en el núcleo del anticlinal que es cortado por fallas inversas, formando una estructura de lámina de sal paralela a la estratificación. Las estructuras observadas, como almohadas de sal, glaciares de sal, láminas de sal y lenguas de sal, indican estilos estructurales compresivos de madurez intermedia a alta. El modelo discontinuo resultó ser el más coherente, ya que la rampa lateral no presentaba niveles evaporíticos, lo cual coincide con la observación en la naturaleza. La Falla transversal del Neusa se representó en el modelo como la rampa lateral, explicando la localización de los niveles salinos en la zona sur del Anticlinal de Zipaquirá. Por último, la evolución de los modelos mostró rotaciones horarias cercanas a la rampa lateral, consistentes con los patrones de rotaciones horarias reportados en la zona axial de la Cordillera Oriental.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT Sedimentary sequences containing evaporitic levels exhibit complex three-dimensional structures due to halokinetic movements known as salt tectonics. In the Anticlinal de Zipaquirá, located in the Cordillera Oriental of Colombia, saline levels are reported within the Lower Cretaceous units. This study conducted a structural analysis of the evolution of the Anticlinal de Zipaquirá, based on analogue models that simulate the relationship between salt tectonics and the transverse zones that bound and segment this structure. The models were constructed on a sandbox-type deformation table, maintaining a constant displacement velocity. The models simulate basement anisotropies using a rigid wooden block consisting of two frontal ramps inclined at 30° connected by a lateral ramp. Adjacent to this block, a layer of non-newtonian fluid and variable-colored fine quartz sand layers were arranged. Three configurations were implemented with different distributions of the non-newtonian fluid layer: A) thin continuous, B) discontinuous, and C) thick continuous. At least 15 experiments were conducted for each configuration. The results of the analogue modeling showed that the salt body in the core of the anticline is cut by reverse faults, forming a parallel salt sheet structure to the stratification. The observed structures, such as salt pillows, salt glaciers, salt sheets, and salt tongues, indicate compressive structural styles of intermediate to high maturity. The discontinuous model proved to be the most coherent since the lateral ramp did not exhibit evaporitic levels, aligning with observations in nature. The Neusa transverse Fault was represented by the lateral ramp in the model, explaining the localization of saline levels in the southern zone of the Anticlinal de Zipaquirá. Finally, the evolution of the models revealed clockwise rotations near the lateral ramp, consistent with the reported patterns of clockwise rotations in the axial zone of the Cordillera Oriental.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[modelos análogos]]></kwd>
<kwd lng="es"><![CDATA[fallas]]></kwd>
<kwd lng="es"><![CDATA[rampas]]></kwd>
<kwd lng="es"><![CDATA[tectónica salina]]></kwd>
<kwd lng="es"><![CDATA[Cordillera Oriental de Colombia]]></kwd>
<kwd lng="es"><![CDATA[Anticlinal de Zipaquirá]]></kwd>
<kwd lng="en"><![CDATA[analogous models]]></kwd>
<kwd lng="en"><![CDATA[faults]]></kwd>
<kwd lng="en"><![CDATA[ramps]]></kwd>
<kwd lng="en"><![CDATA[salt tectonics]]></kwd>
<kwd lng="en"><![CDATA[Eastern Cordillera of Colombia]]></kwd>
<kwd lng="en"><![CDATA[Zipaquirá Anticline]]></kwd>
</kwd-group>
</article-meta>
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