<?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>S1026-87742022000300293</article-id>
<article-id pub-id-type="doi">10.22201/cgeo.20072902e.2022.3.1704</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Tiempos de acumulación de carbón en México con especial énfasis en la Cuenca de Sabinas México, donde se proporcionan nuevos datos geocronológicos]]></article-title>
<article-title xml:lang="en"><![CDATA[Review of the times of coal accumulation in Mexico with special emphasis on the Sabinas basin, Mexico, where geochronological data are provided]]></article-title>
</title-group>
<contrib-group>
<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[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[Camprubí]]></surname>
<given-names><![CDATA[Antoni]]></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[Iriondo]]></surname>
<given-names><![CDATA[Alexander]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
<xref ref-type="aff" rid="Aaf"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Enciso-Cárdenas]]></surname>
<given-names><![CDATA[Juan Josué]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[González Carrillo]]></surname>
<given-names><![CDATA[Fabiola]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Vázquez Ramírez]]></surname>
<given-names><![CDATA[Juan Tomás]]></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[Querétaro Qro]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad Nacional Autónoma de México Instituto de Geología ]]></institution>
<addr-line><![CDATA[Coyoacán Ciudad de México]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,University of Arizona Department of Geociences ]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
<country>USA</country>
</aff>
<aff id="Af4">
<institution><![CDATA[,Universidad Autónoma de Coahuila Centro de Investigación en Geociencias Aplicadas ]]></institution>
<addr-line><![CDATA[Nueva Rosita Coahuila de Zaragoza]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af5">
<institution><![CDATA[,Universidad Autónoma de Coahuila Escuela Superior de Ingeniería Lic. Adolfo López Mateos ]]></institution>
<addr-line><![CDATA[Nueva Rosita Coahuila de Zaragoza]]></addr-line>
<country>Mexico</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>00</month>
<year>2022</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>00</month>
<year>2022</year>
</pub-date>
<volume>39</volume>
<numero>3</numero>
<fpage>293</fpage>
<lpage>307</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1026-87742022000300293&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1026-87742022000300293&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1026-87742022000300293&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN En México, se han identificado en el tiempo y espacio diferentes épocas de acumulacio&#769;n de materia orga&#769;nica, que han dado origen a distintas cuencas carboni&#769;feras como en el Tria&#769;sico la Cuenca de Barrancas en la Regio&#769;n Carboni&#769;fera de San Marcial en Sonora; en el Jura&#769;sico Medio y Tardi&#769;o la Cuenca de Tlaxiaco en Oaxaca; y en el Creta&#769;cico superior las cuencas de Chihuahua y Sabinas, estas u&#769;ltimas objeto de este estudio en este trabajo. En el Terciario se tienen varias manifestaciones de carbón, las más importantes son las de la región carbonífera de Colombia-San Ignacio, Estados de Tamaulipas, Coahuila y Nuevo León. La región carbonífera de Sabinas aporta más del 90 % de la producción nacional de carbón. La Cuenca de Sabinas posee un área de 37000 km2, y su origen está relacionado con la apertura del Proto-Golfo de México y su &#8220;cierre tectónico&#8221; con la Orogenia Larámide, estando delimitada por altos estructurales como son la Península de Coahuila, la plataforma Burro-Peyotes y el arco de Tamaulipas y las fallas como La Babia y San Marcos. En esta cuenca está la Formación Olmos, también conocida como &#8220;Formación del Carbón&#8221;, cuyo origen pasa por dos períodos de formación: 1) un ambiente palustre donde la flora fue abundante y permitió el depósito de turba con espesores y calidad variables; 2) un ambiente continental y transicional: intermarea superior, laguna marginal, pantano y planicies aluviales. Los estudios paleobotánicos, de polen y esporas, la han definido como un sistema deltaico del Cretácico Superior en un ambiente climático subtropical. Por su posición estratigráfica, estructural y distribución espacial, además de producir carbón, es un play favorable para gas. Los mantos de carbón en la cuenca de Sabinas presentan un horizonte &#8220;guía&#8221; de toba que nos ha permitido en este trabajo datar la época de acumulación del carbón por el método de U-Pb en zircones, dado que estos son refractarios para la temperatura de diagénesis a la que fueron sometidas las diferentes plantas originales que conforman los mantos de carbón de la cuenca. Su edad determinada por el método U-Pb en zircones en este trabajo fue de 76.1 ± 1.2 Ma, este dato es congruente con la actividad magmática regional, dado que la subducción al Occidente de área de estudio ha estado activa durante todo el Cretácico hasta el Terciario con la generación de magmas intrusivos y efusivos en lo que se conoce como el Arco Magmático Laramídico Mexicano, conformado en gran parte por la Sierra Madre Occidental, es así que rocas volcanoclásticas has sido reportadas para el Cretácico Superior, tanto relacionadas a mantos de carbón como eventos distales provenientes del Occidente de México, una de las provincias volcanoclásticas más grandes del mundo, en donde se reportan numerosos datos que concuerdan con la edad determinada en este trabajo. En este sentido la cuenca de Sabinas, y sus mantos de carbón, son un buen referente para la combinación de métodos de investigación geocronológica como los paleobotánicos y geocronológicos de decaimiento radioactivo.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT Different periods of coal accumulation have been identified in time and space in Mexico. Some examples are the Triassic of Sonora in the San Marcial coal region, the Middle and Late Jurassic in the Tlaxiaco basin, the Lower Cretaceous in the Cabullona Basin in Sonora and the Upper Cretaceous in the Chihuahua and Sabinas Basin (object of the present work). In the Tertiary, there are several manifestations of coal, the most important are those of the coal region of Colombia-San Ignacio, States of Tamaulipas, Coahuila, and Nuevo León. The Sabinas Basin coal region contributes more than 90 % of the national coal production. The Sabinas Basin has an area of 37000 km2, and its origin is related to the opening of the Proto-Gulf of Mexico and its "tectonic closure&#8221;, with the Laramide Orogeny. The Basin is being delimited by structural highs such as the Coahuila Peninsula, the Burro-Peyotes and the Tamaulipas arch, and faults such as La Babia and San Marcos. Within this basin is the Olmos Formation, also known as the &#8220;Coal Formation&#8221;, whose origin goes through two formation periods: 1) a marshy environment where the flora was abundant and allowed the deposit of peat with variable thicknesses and quality; 2) a continental and transitional environment: upper intertidal, marginal lagoon, swamp and alluvial plains. Paleobotanical studies of pollen and spores have defined it as a deltaic system of the Upper Cretaceous in a subtropical climatic environment. Due to its stratigraphic characteristics, structural position, spatial distribution and its production of coal, the Olmos formation is a favorable play for gas. The coal mantles in the Sabinas basin present a &#8220;guide-layer&#8221; of volcanic tuff that allowed us to date the time of coal accumulation by U-Pb method in zircons. These minerals are refractory, so the age of deposit is not modified at temperature of diagenesis during the transformation of organic matter to coal. The age determined by the U-Pb method in zircons is 76.1 ± 1.2 Ma. This data is consistent with the regional magmatic activity of the area. The subduction to the west of the study area was active from the Cretaceous until the Tertiary with the generation of intrusive and effusive magmas known as the Mexican Laramide Magmatic Arc, which made up the Sierra Madre Occidental. The Laramie magmatic Arc is one of the largest volcanoclastic provinces in the world, and numerous age data have been reported similar the reported in the present work. So, the Sabinas basin, and its coal seams, are a good reference for the combination of geochronological research methods such as paleobotanical and radioactive decay geochronological methods.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[Sabinas]]></kwd>
<kwd lng="es"><![CDATA[Formación Olmos]]></kwd>
<kwd lng="es"><![CDATA[carbón]]></kwd>
<kwd lng="es"><![CDATA[toba]]></kwd>
<kwd lng="es"><![CDATA[geocronología U-Pb en zircones]]></kwd>
<kwd lng="en"><![CDATA[Sabinas]]></kwd>
<kwd lng="en"><![CDATA[Olmos Formation]]></kwd>
<kwd lng="en"><![CDATA[coal]]></kwd>
<kwd lng="en"><![CDATA[tuff]]></kwd>
<kwd lng="en"><![CDATA[geochronology U-Pb in zircons.]]></kwd>
</kwd-group>
</article-meta>
</front><back>
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