<?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>S1026-87742024000300249</article-id>
<article-id pub-id-type="doi">10.22201/igc.20072902e.2024.3.1832</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Restauración y balanceo estructural del campo supergigante Cantarell-Sihil]]></article-title>
<article-title xml:lang="en"><![CDATA[Restoration and structural balancing of the Cantarell-Sihil supergiant field]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Borges-Santana]]></surname>
<given-names><![CDATA[Oscar]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Padilla y Sánchez]]></surname>
<given-names><![CDATA[Ricardo José]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad Nacional Autónoma de México Facultad de Ingeniería División de Ingeniería en Ciencias de la Tierra]]></institution>
<addr-line><![CDATA[Ciudad de México ]]></addr-line>
<country>Mexico</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>00</month>
<year>2024</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>00</month>
<year>2024</year>
</pub-date>
<volume>41</volume>
<numero>3</numero>
<fpage>249</fpage>
<lpage>273</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1026-87742024000300249&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1026-87742024000300249&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1026-87742024000300249&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN En el presente trabajo se presenta la restauración y balanceo de secciones de la estructura plegada Cantarell-Sihil, sureste del Golfo de México. Esto se realizó a través de la metodología de secciones balanceadas, interpretadas con el software Petrel, de un cubo sísmico OBC Kirchhoff, en profundidad, apoyados en líneas sísmicas aleatorias, registros de pozos y cimas geológicas reportadas en varios pozos productores del área de estudio. A parir de la interpretación sísmica se utilizó el software Move para la restauración secuencial de dos secciones, una orientada en dirección N-S y la otra E-W, desde el estado de deformación actual hasta el estado inicial (Calloviano). Los resultados obtenidos indican que la historia geológica de la deformación de la cabalgadura de Cantarell ocurre en tres episodios tectónicos importantes: 1) evento de extensión desde el Jurásico al Cretácico y la consecuente sedimentación de la Sal del Calloviano y carbonatos de espesor variable. Las zonas de menos espesor situadas en la cima de la almohada salina representan el punto de rompimiento que dio origen a la falla Sihil, y que a su vez sirvió como superficie de despegue para el inicio de la deformación y origen de la estructura de Cantarell. 2) Evento de contracción Oligoceno, cuando ocurre el primer acortamiento de ~4 km que da inicio al cabalgamiento del bloque Cantarell, previo al evento Chiapaneco, y 3) evento extensivo durante el Plioceno hasta el Reciente evidenciado por la aparición de fallas normales en las zonas adyacentes a Cantarell. El resultado final de restauración reveló que las etapas iniciales de la deformación de la cabalgadura de Cantarell no están asociadas al evento Chiapaneco como ha sido sugerido en los últimos años, y que la secuencia sedimentaria de la región de Cantarell tuvo un acortamiento de aproximadamente 11 km, el cual influyó en la formación del campo supergigante Cantarell-Sihil, en el sureste de México.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT The present work provides a series of restored cross-sections of the Cantarell-Sihil folded structure, southeastern Gulf of Mexico. This was done with Petrel software, from an OBC Kirchhoff seismic cube at depth, supported by several random seismic lines, well logs and geological contacts reported in several producing wells in the study area. Based on the seismic interpretation, we used the Move software for the sequential restoration of two sections, one oriented N-S and the other E-W, from the current deformed state to the initial state (Callovian). The results obtained indicate that the development of the Cantarell Ridge took place in three tectonic episodes: 1) A Jurassic to Cretaceous extension event that resulted in the deposition of evaporites of Callovian age and carbonates of variable thickness. Carbonate successions diminish in thickness laterally and reach a minimum atop the salt pillow. This slender succession offered little resistance and buckled under compression during the Tertiary, giving rise to the Sihil fault, which in turn served as a detachment surface for the beginning of the deformation and origin of the Cantarell structure. 2) An Oligocene contraction event of ~4 km occurs, which initiates the Cantarell thrust, prior to the Chiapaneco event. And 3) an extension event during the Pliocene to the Recent evidenced by the initiation of normal faults in the areas adjacent to Cantarell. The final restoration revealed that the initial stages of the deformation of the Cantarell ridge were not associated with the Chiapaneco event as has been suggested in recent years, and that the sedimentary sequence of the Cantarell region had a shortening of approximately 11 km, which influenced the formation of the Cantarell-Sihil supergiant oil field in southeastern Mexico.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[restauración]]></kwd>
<kwd lng="es"><![CDATA[balanceo]]></kwd>
<kwd lng="es"><![CDATA[secciones estructurales]]></kwd>
<kwd lng="es"><![CDATA[campo supergigante]]></kwd>
<kwd lng="es"><![CDATA[Cabalgadura Cantarell]]></kwd>
<kwd lng="es"><![CDATA[campo Cantarell-Sihil]]></kwd>
<kwd lng="es"><![CDATA[México]]></kwd>
<kwd lng="en"><![CDATA[restoration]]></kwd>
<kwd lng="en"><![CDATA[balancing]]></kwd>
<kwd lng="en"><![CDATA[structural cross section]]></kwd>
<kwd lng="en"><![CDATA[supergiant oil field]]></kwd>
<kwd lng="en"><![CDATA[Cantarell thrust]]></kwd>
<kwd lng="en"><![CDATA[Cantarell-Sihil field]]></kwd>
<kwd lng="en"><![CDATA[Mexico]]></kwd>
</kwd-group>
</article-meta>
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