<?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>S1405-33222017000300711</article-id>
<article-id pub-id-type="doi">10.18268/bsgm2017v69n3a11</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[The Triassic/Jurassic boundary and the Jurassic stratigraphy and biostratigraphy of northern Sonora, northwest Mexico]]></article-title>
<article-title xml:lang="es"><![CDATA[El límite Triásico/Jurásico, y estratigrafía y bioestratigrafía del Jurásico del norte de Sonora, noroeste de México]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[González-León]]></surname>
<given-names><![CDATA[Carlos M.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Stanley Jr.]]></surname>
<given-names><![CDATA[George D.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Lawton]]></surname>
<given-names><![CDATA[Timothy F.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Pálfy]]></surname>
<given-names><![CDATA[József]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Hodges]]></surname>
<given-names><![CDATA[Montana S.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad Nacional Autónoma de México Instituto de Geología Estación Regional del Noroeste]]></institution>
<addr-line><![CDATA[ Sonora]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,University of Montana Paleontology Center  ]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
<country>USA</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Universidad Nacional Autónoma de México Centro de Geociencias ]]></institution>
<addr-line><![CDATA[ Querétaro]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af4">
<institution><![CDATA[,Eötvös Loránd University Department of Physical and Applied Geology ]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
<country>Hungary</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>00</month>
<year>2017</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>00</month>
<year>2017</year>
</pub-date>
<volume>69</volume>
<numero>3</numero>
<fpage>711</fpage>
<lpage>738</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1405-33222017000300711&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1405-33222017000300711&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1405-33222017000300711&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract The Triassic and Jurassic geology of northern Sonora encompasses important events that are linked to the late Paleozoic history of the region. The fossiliferous El Antimonio Group in the Sierra del Álamo includes the upper Permian-Triassic Antimonio, and Río Asunción formations and the Hettangian-Sinemurian Sierra de Santa Rosa Formation. These formations consist of upward-fining sequences from I to XIV that represent fluvial to shallow and deep marine environments of deposition. The Triassic/Jurassic boundary in this region is a hiatus represented by a disconformity between sequence IX of the Río Asunción formations and sequence X of the Sierra de Santa Rosa Formation. The shallow to deep marine succession of the Sierra de Santa Rosa composes the upper part of the Sierra de Santa Rosa Formation that ranges in age from late Sinemurian to early Pliensbachian. Ages of the Permian to Triassic plutonic rocks of northwesternmost Sonora, the Mojave Desert and the Jurassic continental margin Nazas arc that crossed through northern Sonora, are also well recorded by igneous clasts and detrital zircon grains that have been dated from the El Antimonio Group and other Jurassic formations of this region. The upper Oxfordian-lower Tithonian Cucurpe Formation in north-central Sonora recorded the onset of continental extension and incursion of marine waters from the Gulf of Mexico into northwestern Mexico, once activity of the Jurassic magmatic arc ended.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen La historia triásica y jurásica del norte de Sonora abarca importantes eventos que están vinculados a la historia del Paleozoico tardío de la región. El Grupo El Antimonio que aflora en la Sierra del Álamo incluye las formaciones Antimonio y Río Asunción del Pérmico tardío Triásico Tardío y a la Formación Sierra de Santa Rosa que tiene edad Hettangiana-Sinemuriana. Estas formaciones están compuestas por secuencias grano-decrecientes que se han numerado de la I a la XIV y representan ambientes de depósito que van de fluviales a marinos profundos. El límite Triásico/ Jurásico en esta región es un hiato representado por una disconformidad entre la secuencia IX de la Formación Río Asunción y la secuencia X de la Formación Sierra de Santa Rosa. La sucesión marina somera a marina profunda de la Formación Sierra de Santa Rosa que aflora en la sierra del mismo nombre constituye la parte superior de dicha formación cuya edad se extiende del Sinemuriano tardío al Pliensbachiano temprano. Las edades del magmatismo Pérmico y Triásico que ocurrió en el noroeste de Sonora y en el desierto Mojave del suroeste de Estados Unidos, así como las del magmatismo del arco continental Nazas que atravesó el norte de Sonora durante el Jurásico, están bien registradas en edades obtenidas en clastos ígneos y en circones detríticos que se han fechado del Grupo El Antimonio y otras formaciones Jurásicas de la región. La Formación Cucurpe del Jurásico Tardío (Oxfordiano tardío - Titoniano temprano) registra, en el centro-norte de Sonora, el inicio de una extensión continental y la incursión de aguas marinas del Golfo de México una vez que concluyó la actividad del arco magmático jurásico.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[Triassic-Jurassic]]></kwd>
<kwd lng="en"><![CDATA[El Antimonio Group]]></kwd>
<kwd lng="en"><![CDATA[Sierra de Santa Rosa Formation]]></kwd>
<kwd lng="en"><![CDATA[Cucurpe Formation]]></kwd>
<kwd lng="en"><![CDATA[biostratigraphy]]></kwd>
<kwd lng="es"><![CDATA[Triásico-Jurásico]]></kwd>
<kwd lng="es"><![CDATA[Grupo El Antimonio]]></kwd>
<kwd lng="es"><![CDATA[Formación Sierra de Santa Rosa]]></kwd>
<kwd lng="es"><![CDATA[Formación Cucurpe]]></kwd>
<kwd lng="es"><![CDATA[Bioestratigrafía]]></kwd>
</kwd-group>
</article-meta>
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