<?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>S1405-33222020000200008</article-id>
<article-id pub-id-type="doi">10.18268/bsgm2020v72n2a151219</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Diagenésis de la Formación Eagle Ford y sus marcadores térmicos como productora de gas no convencional]]></article-title>
<article-title xml:lang="en"><![CDATA[Diagenesis of the Eagle Ford Formation and its thermal markers as a producer of unconventional gas]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[González Betancourt]]></surname>
<given-names><![CDATA[Aurea Yahaira]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[González Partida]]></surname>
<given-names><![CDATA[Eduardo]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Piedad Sánchez]]></surname>
<given-names><![CDATA[Noé]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Carrillo Chávez]]></surname>
<given-names><![CDATA[Alejandro]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[González Ruiz]]></surname>
<given-names><![CDATA[Luis Eduardo]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[González Ruiz]]></surname>
<given-names><![CDATA[Daniel]]></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 ]]></institution>
<addr-line><![CDATA[Juriquilla Querétaro]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Academia de Investigacion A.C. Innovacion Tecnológica Aplicada a las Geociencias ]]></institution>
<addr-line><![CDATA[ Hidalgo]]></addr-line>
<country>México</country>
</aff>
<aff id="Af4">
<institution><![CDATA[,Geologia Mineria y Consultoria, S.A. de C.V.  ]]></institution>
<addr-line><![CDATA[ Queretaro]]></addr-line>
<country>México</country>
</aff>
<aff id="Af5">
<institution><![CDATA[,Centro Nacional de Investigaciones Avanzadas en Petrofísica CENIAPET, S. A. de C. V.  ]]></institution>
<addr-line><![CDATA[ Querétaro]]></addr-line>
<country>México</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>00</month>
<year>2020</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>00</month>
<year>2020</year>
</pub-date>
<volume>72</volume>
<numero>2</numero>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1405-33222020000200008&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1405-33222020000200008&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1405-33222020000200008&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen En México existen unidades geológicas compuestas por sedimentos de grano cfmuy fino y ricas en materia orgánica, que podrían considerarse como recursos potenciales de hidrocarburos. Entre ellas se encuentra la Formación Eagle Ford (Cenomaniano Tardío-Turoniano), la cual es el objeto de estudio en este trabajo. Dicha formación está localizada dentro de la Paleocuenca de Sabinas y sobre la Paleoplataforma Burro-Peyotes, en el estado de Coahuila. Anteriormente se ha definido que representa un sistema transgresivo depositado en un ambiente marino nerítico-medio con valores de carbón orgánico total (COT) entre 0.5 y 8% y con materia orgánica del tipo II predominante, por lo que podría considerarse como un posible recurso de hidrocarburos no convencional. Para ello se considera que un reservorio de lutitas gasíferas (shale gas) debe cumplir con ciertos requisitos, como: 1) Riqueza orgánica (&gt;2% de COT), 2) tipo de kerógeno II o III, 3) valores de reflectancia de la vitrinita mayor a 1.2% Ro (0.7% para shale oil), 4) espesor mayor a 30 m y gran extensión, 5) fracturabilidad (&lt;40% de arcillas o ausencia de arcillas expandibles) o la presencia de un sistema de microfisuras, 6) sobrepresión, 7) profundidad adecuada, 8) heterogeneidad, entre otras. Con el objetivo de determinar el grado de madurez térmico de esta formación, se realizó un muestreo sistemático en afloramientos del estado de Coahuila para el análisis de estratigrafía a detalle (columnas CSI, CSII, CSV) y microtermometría de inclusiones fluidas. Los resultados ratifican que la Formación Eagle Ford es una secuencia sedimentaria rica en materia orgánica, compuesta localmente por lutita calcárea carbonosa con estratificación laminar que alterna a caliza arcillosa (mudstone-wackestone) y caliza clástica- bioclástica (packstone-grainstone). Respecto a las alteraciones diagenéticas, la porosidad de origen primario se ve afectada por los procesos de compactación y precipitación de cementos, también se generó una microporosidad secundaria debido al desarrollo de neomorfismo, dolomitización, fracturas y estilolitización. Además, se determinó que las temperaturas de homogeneización (Th) de inclusiones fluidas que alcanzó esta formación varían entre los 65 °C y 125 °C, lo que la sitúa en la etapa catagenética de la generación de petróleo y gas húmedo. Asimismo, se observó que la evolución térmica de inclusiones fluidas en la cuenca no es homogénea.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT There are several organic matter-rich shale geologic formations in Mexico that could be considered non-conventional potential oil reservoirs; one of those formations is the Eagle Ford Formation (Late Cenomanian - Turonian), aim of this study. The Eagle Ford Formation is located within the Sabinas paleobasin and along the Burros-Peyote paleoplatform, in the Coahuila State. This formation has been previously described as a transgression system deposited in a shallow marine environment with a total organic carbon between 0.5 to 8% with type II organic matter. For these reasons, it could be considered a potential source for non-conventional hydrocarbons. Therefore, it is considered that a reservoir of shale gas must have certain requirements, such as: 1) high total organic carbon (&gt; 2% of COT), 2) presence of types II and III kerogen, 3) vitrinite reflectance values greater than 1.2% Ro (0.7% for shale oil), 4) thickness greater than 30 m and large extension, 5) fracturability (&lt;40% clays or absence of expandable clays) or the presence of a microcracking system, 6) overpressure, 7) adequate depth, 8) heterogeneity, and others. A systematic sampling was carried on outcrops of Coahuila State with the goal to determine the thermal maturity degree of the Eagle Ford Formation using a detailed stratigraphic analysis of three columns (CSI, CSII and CSV) and micro-thermometric of fluid inclusions. Our results indicate that the Eagle Ford Formation is a sedimentary sequence rich in organic matter, locally composed of carbonaceous carbonate shale in laminar stratification alternating with shaly limestone (mudstone-wackestone) and clastic o bioclastic limestone (packstone-grainstone). Regarding the diagenetic alteration, primary porosity is affected by compaction and cementation processes. However, it was also observed a secondary micro-porosity development due to neomorphism, dolomitization, fracturing and stylolitization processes. Measured homogenization temperatures (Th) in fluid inclusions are between 65 °C and 125 °C, reaching the temperature window to generate oil and humid gas. The thermal evolution through its facies changes in the basin is not homogeneous. Our results indicate that the Eagle Ford Formation is a sedimentary sequence rich in organic matter, locally composed of carbonaceous carbonate shale in laminar stratification alternating with shaly limestone (mudstone-wackestone) and clastic o bioclastic limestone (packstone-grainstone).]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[Recurso no convencional]]></kwd>
<kwd lng="es"><![CDATA[petrografía]]></kwd>
<kwd lng="es"><![CDATA[inclusiones fluidas]]></kwd>
<kwd lng="es"><![CDATA[gas]]></kwd>
<kwd lng="es"><![CDATA[diagénesis]]></kwd>
<kwd lng="en"><![CDATA[Non-Conventional hydrocarbon reservoir]]></kwd>
<kwd lng="en"><![CDATA[petrography]]></kwd>
<kwd lng="en"><![CDATA[fluid inclusions]]></kwd>
<kwd lng="en"><![CDATA[gas]]></kwd>
<kwd lng="en"><![CDATA[diagenesis]]></kwd>
</kwd-group>
</article-meta>
</front><back>
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