<?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>S1405-33222022000200113</article-id>
<article-id pub-id-type="doi">10.18268/bsgm2022v74n2a230222</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Deformación del Cretácico tardío en el límite de la Mesa Central y la Sierra Madre Oriental, centro de México]]></article-title>
<article-title xml:lang="en"><![CDATA[Late Cretaceous deformation at the border between the Mesa Central and the Sierra Madre Oriental, central Mexico]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Cid-Villegas]]></surname>
<given-names><![CDATA[Gonzalo]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Alaniz-Álvarez]]></surname>
<given-names><![CDATA[Susana Alicia]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Xu]]></surname>
<given-names><![CDATA[Shunshan]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Vásquez-Serrano]]></surname>
<given-names><![CDATA[Alberto]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<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-group>
<aff id="Af1">
<institution><![CDATA[,aff1  ]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
<country>México</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad Nacional Autónoma de México Centro de Geociencias ]]></institution>
<addr-line><![CDATA[ Querétaro]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Universidad Nacional Autónoma de México Instituto de Geología ]]></institution>
<addr-line><![CDATA[ CDMX]]></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>74</volume>
<numero>2</numero>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1405-33222022000200113&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1405-33222022000200113&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1405-33222022000200113&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN En el centro de México se han identificado dos eventos tectónicos importantes del Cretácico: la acreción del Terreno Guerrero (Cretácico Temprano) y la formación del Orógeno Mexicano (Cretácico Tardío-Paleógeno). Ambos eventos presentan una dirección de transporte tectónico al noreste en el centro del país, y han sido estudiados tanto en la Mesa Central, como en la Sierra Madre Oriental. No obstante, pocos trabajos han caracterizado la deformación contractiva en el límite entre ambas provincias. Con el fin de contribuir a una mejor comprensión de la deformación del Cretácico Tardío en el centro de México, el presente trabajo se enfoca en el límite de ambas provincias, especialmente en las localidades Juriquilla, San Miguel de Allende y la Sierra de los Cuarzos. Los objetivos de este trabajo fueron: a) Identificar la deformación contractiva de las rocas mesozoicas de la zona de estudio. b) Determinar variaciones en la dirección de transporte tectónico de la zona de estudio con respecto a la Mesa Central y Sierra Madre Oriental. En este estudio se reportan nuevos datos estructurales y edades U-Pb en granos de circón detrítico. Se discute sobre la posibilidad de tener dos eventos de deformación contractiva. El evento D1 se infiere contemporáneo a la acreción del Terreno Guerrero y se observa en las rocas más antiguas de Sierra de los Cuarzos. Por su parte, las edades máximas de depósito obtenidas en San Miguel de Allende y Juriquilla, 110.2 ± 0.8 Ma y 110.5 ± 0.9 Ma (Albiano temprano), respectivamente, limitan la edad de la deformación D2, siendo posterior a los ~110 Ma. Por lo tanto, esta deformación resulta contemporánea a la formación del Orógeno Mexicano. El evento D2 se observa en las tres áreas. Mediante el análisis estructural se determinó que D1 tiene una dirección de transporte al sureste, mientras que D2 presenta una dirección de transporte general al oeste-suroeste o suroeste. Estas direcciones de transporte difieren al de la acreción del Terreno Guerrero y al de la formación del Orógeno Mexicano. Esta diferencia en la dirección de transporte podría ser producto de retrodeformación, y/o heterogeneidades en el basamento.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT In central Mexico, two important Cretaceous tectonic events have been identified: the accretion of the Guerrero Terrain (Early Cretaceous) and the beginning of the Mexican Orogen (Late Cretaceous-Paleogene). Both events present a direction of tectonic transport to the northeast in the center of México, and they have been studied both in the Mesa Central and in the Sierra Madre Oriental. However, little study has characterized the contractile deformation in the border between both provinces. In order to contribute to a better understanding of the Late Cretaceous deformation in central Mexico, this research focuses on the border of both provinces, especially in the Juriquilla, San Miguel de Allende localities, and Sierra de los Cuarzos. The objectives of this research were a) Identify the contractile deformation of the Mesozoic rocks in the study area. b) Determine variations in the direction of tectonic transport of the study area concerning the Mesa Central and Sierra Madre Oriental. In this research, new structural data and U-Pb ages in detrital zircon grains are reported. The possibility of having two contractive deformation events is discussed. The D1 event is inferred contemporary to the accretion of the Guerrero Terrain and is observed in the oldest rocks of Sierra de los Cuarzos. On other hand, the maximum deposit ages obtained in San Miguel de Allende and Juriquilla, 110.2 ± 0.8 Ma and 110.5 ± 0.9 Ma (Early Albian), respectively, limit the age of the D2 deformation, being after ~ 110 Ma. Therefore, this resulting deformation contemporaneous with the formation of the Mexican Orogen. Event D2 is observed in all three areas. Through the structural analysis it was determined that D1 has a direction of transport to the southeast, while D2 has a direction of transport to the west-southwest or southwest. These transport directions differ from that of the Guerrero Terrain accretion and from the formation of the Mexican Orogen. This difference in the direction of transport could be the product of retrodeformation, and or heterogeneities in the basement.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[Deformación contractiva del Cretácico Tardío]]></kwd>
<kwd lng="es"><![CDATA[análisis estructural]]></kwd>
<kwd lng="es"><![CDATA[transporte tectónico]]></kwd>
<kwd lng="es"><![CDATA[geocronología U-Pb]]></kwd>
<kwd lng="es"><![CDATA[centro de México]]></kwd>
<kwd lng="en"><![CDATA[Cretaceous contractive deformation]]></kwd>
<kwd lng="en"><![CDATA[structural analysis]]></kwd>
<kwd lng="en"><![CDATA[tectonic transport]]></kwd>
<kwd lng="en"><![CDATA[U-Pb geochronology]]></kwd>
<kwd lng="en"><![CDATA[central Mexico]]></kwd>
</kwd-group>
</article-meta>
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<surname><![CDATA[Nieto-Samaniego]]></surname>
<given-names><![CDATA[Á.F.]]></given-names>
</name>
<name>
<surname><![CDATA[Alaniz-Álvarez]]></surname>
<given-names><![CDATA[S.A.]]></given-names>
</name>
<name>
<surname><![CDATA[Cerca-Martínez]]></surname>
<given-names><![CDATA[L.M.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[Structural analysis of a relay ramp in the Querétaro graben, central Mexico: implications for relay ramp development]]></article-title>
<source><![CDATA[Revista Mexicana de Ciencias Geológicas]]></source>
<year>2011</year>
<volume>28</volume>
<page-range>275-89</page-range></nlm-citation>
</ref>
</ref-list>
</back>
</article>
