<?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>S1026-87742015000300455</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Características geoquímicas y significado tectónico del complejo de diques y domos félsicos del Paleoceno-Eoceno de La Tesorera, Zacatecas, en la Mesa Central, México]]></article-title>
<article-title xml:lang="en"><![CDATA[Geochemical characteristics and tectonic significance of the Paleocene-Eocene felsic diques and dome complex of La Tesorera, Zacatecas, Mesa Central, México]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Tristán-González]]></surname>
<given-names><![CDATA[Margarito]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Aguillón-Robles]]></surname>
<given-names><![CDATA[Alfredo]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Barboza-Gudiño]]></surname>
<given-names><![CDATA[José Rafael]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Cruz-Márquez]]></surname>
<given-names><![CDATA[Judith]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[García-Arreola]]></surname>
<given-names><![CDATA[María Elena]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Bellon]]></surname>
<given-names><![CDATA[Hervé]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Franzetti]]></surname>
<given-names><![CDATA[Marcaurelio]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Labarthe-Hernández]]></surname>
<given-names><![CDATA[Guillermo]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad Autónoma de San Luis Potosí Instituto de Geología ]]></institution>
<addr-line><![CDATA[San Luis Potosí S.L.P.]]></addr-line>
<country>México</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad Autónoma de San Luis Potosí Facultad de Ingeniería Posgrado en Geología Aplicada]]></institution>
<addr-line><![CDATA[San Luis Potosí S.L.P.]]></addr-line>
<country>México</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Université de Bretagne Occidentale Institut Universitaire Européen de la Mer ]]></institution>
<addr-line><![CDATA[Brest Cedex ]]></addr-line>
<country>Francia</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>12</month>
<year>2015</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>12</month>
<year>2015</year>
</pub-date>
<volume>32</volume>
<numero>3</numero>
<fpage>455</fpage>
<lpage>474</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1026-87742015000300455&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1026-87742015000300455&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1026-87742015000300455&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN El Complejo Ígneo La Tesorera (CIT) está compuesto por una secuencia sedimentaria y vulcanosedimentaria mesozoica perteneciente al terreno Guerrero (TG) así como de sedimentos calcáreos del Cretácico Temprano, deformados por el evento de acortamiento de la orogenia Laramide, y finalmente intrusionado por la Granodiorita Tesorera alrededor de 74 Ma. En el Paleógeno tardío se emplazaron domos volcánicos de lavas dacíticas sobre la granodiorita, seguidos de un conjunto de diques y domos riolíticos extravasados en el rango de 50 y 44 Ma. La secuencia vulcano sedimentaria cretácica se depositó en un ambiente de intraa tras-arco. El desarrollo del arco volcánico de la Sierra Madre Occidental durante el Cretácico Tardío es contemporáneo a la orogenia Laramide y está asociado con el cinturón de pliegues y cabalgaduras de la Sierra Madre Oriental, provocando el ensamble final del terreno Guerrero con el terreno Sierra Madre. En la Granodiorita Tesorera, diques y domos félsicos asociados al arco volcánico de la Sierra Madre Occidental, fueron emplazados a lo largo de fallas y fracturas con orientación NW con anchos variables hasta de 500 m y longitud de ~5 km y sobre las unidades mesozoicas que forman el arco volcánico Asientos-La Tesorera (definido así en este trabajo). Los intrusivos granodioríticos de esta porción meridional de la Mesa Central no presentan deformación contráctil laramídica y se emplazaron en la zona donde se intersectan el sistema de fallas San Luis-Tepehuanes (SFSLT) y el hombro oriental del graben de Aguascalientes. Los diques eocénicos presentan rumbo promedio de N60oW, con inclinación entre 45° y 85° SW, sugiriendo una extensión en dirección ~NE-SW para este periodo de tiempo. De acuerdo con la edad de las rocas volcánicas del área de estudio, la deformación que originó los conductos para el ascenso de las lavas pertenece a las etapas iniciales de la tectónica extensional. La orientación de los diques coincide con la orientación del SFSLT en el tramo San Luis de la Paz-Salinas de Hidalgo, cuya actividad principal se dio durante el Paleógeno. Las características geoquímicas, tales como los elementos mayores y los traza, de las rocas ígneas que conforman el CIT indican que son subalcalinas a alcalinas y peraluminosas, con índice de saturación de alúmina &gt; 1 [Al2O3/(CaO+Na2O+K2O)&gt;1]. Las lavas evolucionaron a partir de un ambiente tectónico de arco volcánico hacia un volcanismo de tipo intraplaca a partir de magmas derivadas del manto por procesos de cristalización fraccionada, dando como resultado una roca intrusiva de composición granodiorítica y rocas extrusivas de composición riolítica que formaron los diques y domos volcánicos.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT The Tesorera igneous complex (CIT) is composed of Mesozoic sedimentary and volcano-sedimentary sequences belonging to the Guerrero terrane (TG) and Early Cretaceous calcareous sediments, deformed by the shortening of the Laramide orogeny and the intrusion of the Tesorera granodiorite around 74 Ma. During Paleogene, dacitic lava domes were emplaced on the granodioritic rock, and were followed by the extrusion of rhyolitic dikes and volcanic domes between 44 to 50 Ma. The Upper Cretaceous volcano-sedimentary sequence was deposited in an intraor back-arc setting. The development of the Sierra Madre Occidental volcanic arc during the Late Cretaceous is contemporary to the Laramide orogeny and is associated with the folds and thrusts belt of the Sierra Madre terrane. The Tesorera Granodiorite pluton, dykes and felsic domes associated with the development of the Sierra Madre Occidental arc were settled along faults and fractures with variable widths up to 500 m and lengths of ~5 km. They were emplaced on the volcano-sedimentary units that form the Asientos-La Tesorera volcanic arc (referred with this name in this work). The granodioritic plutons of this southern part of the Mesa Central do not show laramidic contractile deformation and were emplaced where the San Luis-Tepehuanes Faults System (SLTFS) and the eastern shoulder of the Aguascalientes graben intersect. Structural data of dykes have an average direction N60°W and a dip between 45° and 85° SW, suggesting an extension direction ~ NE-SW. In accordance with the age of the volcanic rocks of the study, the deformation that caused these faults belongs to the initial stages of the extensional tectonics that formed the Basin and Range Province. The orientation of the dykes coincides with the orientation of the SLTFS, mainly at the San Luis de la Paz-Salinas de Hidalgo stretch, whose main activity occurred during the Paleogene time. The geochemical characteristics, like major and trace elements, for the igneous rocks that make up the volcanic complex indicate that they are sub-alkaline to alkaline rocks, and peraluminous with an alumina saturation index &gt;1, [Al2O3/(CaO+Na2O+K2O) &gt; 1]. The lavas evolved from a volcanic arc tectonic environment into an intrapalte volcanism. They were associated with mantle-derived magmas and fractional crystallization processes, and resulted in intrusive rocks of granodioritic composition and extrusive rock of rhyolitic composition that formed dikes and volcanic domes.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[diques y domos félsicos]]></kwd>
<kwd lng="es"><![CDATA[Granodiorita Tesorera]]></kwd>
<kwd lng="es"><![CDATA[volcanismo]]></kwd>
<kwd lng="es"><![CDATA[Mesa Central]]></kwd>
<kwd lng="es"><![CDATA[Complejo Ígneo]]></kwd>
<kwd lng="es"><![CDATA[edades K-Ar]]></kwd>
<kwd lng="en"><![CDATA[felsic dikes and domes]]></kwd>
<kwd lng="en"><![CDATA[Tesorera Granodiorite]]></kwd>
<kwd lng="en"><![CDATA[Mesa Central volcanism]]></kwd>
<kwd lng="en"><![CDATA[igneous complex]]></kwd>
<kwd lng="en"><![CDATA[K-Ar ages]]></kwd>
</kwd-group>
</article-meta>
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