<?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>S1026-87742020000300179</article-id>
<article-id pub-id-type="doi">10.22201/cgeo.20072902e.2020.3.1576</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Arquitectura estratigráfica, ambientes de depósito y geocronología de la Formación Olinalá (Pérmico tardío), noreste de Guerrero, México]]></article-title>
<article-title xml:lang="en"><![CDATA[Stratigraphic architecture, depositional environments and geochronology of the Olinalá Formation (late Permian), northeastern Guerrero, Mexico]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Juárez-Arriaga]]></surname>
<given-names><![CDATA[Edgar]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Murillo-Muñetón]]></surname>
<given-names><![CDATA[Gustavo]]></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]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Instituto Mexicano del Petróleo Dirección de Exploración y Producción ]]></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>2020</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>00</month>
<year>2020</year>
</pub-date>
<volume>37</volume>
<numero>3</numero>
<fpage>179</fpage>
<lpage>196</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1026-87742020000300179&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1026-87742020000300179&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1026-87742020000300179&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN La Formación Olinalá representa una sucesión sedimentaria pérmica marino-continental de ~860 m de espesor, excepcionalmente expuesta en el noreste del estado de Guerrero, en el sur de México. La arquitectura estratigráfica de esta unidad sugiere un sistema de depósito de plataforma tipo rampa homoclinal con sedimentación mixta (terrígena-carbonatada). El análisis U-Pb en granos de circón detrítico obtenidos de dos muestras colectados cerca de la base de la Formación Olinalá permitió determinar una edad máxima de depósito de 268±5 Ma, misma que es consistente con la edad de Wordiano previamente determinada a partir de amonoideos colectados en la base de esta unidad. Esta sucesión sedimentaria contiene una amplia diversidad de facies terrígenas continentales cuyo arreglo arquitectural sugiere el desarrollo de un valle de incisión fluvial de al menos 130 m de profundidad. Por otro lado, las facies terrígenas y carbonatadas marinas sugieren el desarrollo de un sistema de rampa en aguas cálidas bajo condiciones marinas normales. La sucesión de ambientes de depósito en la Formación Olinalá a través del tiempo permite deducir variaciones en el nivel del mar de distinta magnitud que controlaron, en parte, su evolución sedimentaria.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT The Olinalá Formation is a marine-continental Permian sedimentary succession of ~860 m thick, which is exceptionally exposed in the northeast of the Guerrero state, in southern Mexico. The depositional architecture of this sedimentary succession indicates a mixed carbonate-siliciclastic homoclinal ramp system. The U-Pb ages of detrital zircon grains set from two basal sandstones of the Olinalá Formation yielded a weighted mean maximum deposit age of 268±5 Ma, which agrees with a Wordian biostratigraphic age based on ammonoids collected at its base. Wide continental siliciclastic facies diversity was identified in this sedimentary succession that represents a prominent fluvial incision valley of 130 m depth, at least. Instead, the siliciclastic and carbonate marine facies indicate a ramp system developed in warm waters and normal salinity conditions. The superposition of different environments in the Olinalá Formation through time allows us to deduce sea-level changes of a different magnitude, which partly controlled the sedimentary evolution of this unit.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[Pérmico]]></kwd>
<kwd lng="es"><![CDATA[rampa homoclinal]]></kwd>
<kwd lng="es"><![CDATA[facies sedimentarias]]></kwd>
<kwd lng="es"><![CDATA[Formación Olinalá]]></kwd>
<kwd lng="es"><![CDATA[geocronología U-Pb]]></kwd>
<kwd lng="es"><![CDATA[valle de incisión fluvial]]></kwd>
<kwd lng="en"><![CDATA[Permian]]></kwd>
<kwd lng="en"><![CDATA[homoclinal ramp]]></kwd>
<kwd lng="en"><![CDATA[sedimentary facies]]></kwd>
<kwd lng="en"><![CDATA[Olinalá Formation]]></kwd>
<kwd lng="en"><![CDATA[U-Pb geochronology]]></kwd>
<kwd lng="en"><![CDATA[fluvial incision valley]]></kwd>
</kwd-group>
</article-meta>
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