<?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>S1026-87742019000300393</article-id>
<article-id pub-id-type="doi">10.22201/cgeo.20072902e.2019.3.1391</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Edad y origen de la paleocuenca continental de Teocaltiche, México]]></article-title>
<article-title xml:lang="en"><![CDATA[Age and origin of the continental Teocaltiche paleo-basin, Mexico]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[González-Cervantes]]></surname>
<given-names><![CDATA[Norma]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
<xref ref-type="aff" rid="Aaf"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Aranda-Gómez]]></surname>
<given-names><![CDATA[José Jorge]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Carranza-Castañeda]]></surname>
<given-names><![CDATA[Oscar]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Ortega-Obregón]]></surname>
<given-names><![CDATA[Carlos]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad Nacional Autónoma de México Posgrado en Ciencias de la Tierra ]]></institution>
<addr-line><![CDATA[Querétaro Qro]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad Nacional Autónoma de México Centro de Geociencias ]]></institution>
<addr-line><![CDATA[Querétaro Qro]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Universidad Autónoma de Aguascalientes Departamento de Ingeniería Civil ]]></institution>
<addr-line><![CDATA[Aguascalientes Ags]]></addr-line>
<country>Mexico</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>00</month>
<year>2019</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>00</month>
<year>2019</year>
</pub-date>
<volume>36</volume>
<numero>3</numero>
<fpage>393</fpage>
<lpage>410</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1026-87742019000300393&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1026-87742019000300393&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1026-87742019000300393&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN En la región ubicada al este de la parte sudoriental de la Sierra Madre Occidental (SMOc) existió un lago extenso durante parte del Oligoceno y casi todo el Mioceno. El lago se formó en una depresión tectónica, asociada con el graben de Aguascalientes y el semigraben de Teocaltiche. Los sedimentos que rellenaron parcialmente esta cuenca continental incluyen sedimentos epiclásticos derivados de las rocas de la SMOc y de la Mesa Central, precipitados químicos y bioquímicos (caliza de agua dulce) y sedimentos mixtos, así como una proporción pequeña, pero generalizada, de capas de ceniza volcánica de caída, que fueron empleadas para obtener edades de U-Pb en circón. El alcance temporal del relleno de la cuenca es amplio, pues abarca desde el Rupeliano (~28.6 Ma) hasta el Tortoniano (~7.6 Ma). Previamente, con base en fauna fósil se creía que la sucesión era solo del Mioceno tardío. En la parte sur de la SMOc hay varias cuencas de origen tectónico, con orientación NNE, que contuvieron lagos. En al menos tres de ellas (Tlaltenango, Juchipila y Teocaltiche) se sabe, por el carácter de los sedimentos y por sus fósiles del Henfiliano temprano, que hubo lagos de manera simultánea. En el graben de Bolaños, al oeste y paralelo a la cuenca de Tlaltenango, se ha propuesto la existencia de un lago durante el Neógeno, cuyos sedimentos están casi completamente erosionados, por lo que se sabe poco acerca de ellos. Para explicar el bloqueo parcial y simultáneo de los sistemas de drenaje se requiere de una causa común de carácter regional. Las cuatro cuencas tectónicas mencionadas terminan al norte de las depresiones asociadas a los rifts Tepic-Zacoalco o Tula-Chapala. El ajuste isostático en los bloques de piso de estos rifts pudo causar el cierre parcial de los ríos axiales en los grábenes con rumbos NNE y atrapar así los sedimentos. Aunque se desconoce con precisión cuando las cuencas dejaron de ser sistemas acumulativos, se cree, por la ausencia de fósiles del Blancano, que la apertura pudo suceder antes de ~4.75 Ma, valor numérico del inicio de esa etapa faunística. Una causa común probable de la apertura puede ser la invasión marina de una depresión en lo que actualmente es el Golfo de California. La creación de este nuevo nivel base de erosión pudo aumentar considerablemente el gradiente hidráulico en los sistemas fluviales, proveyendo la energía suficiente para remontar al levantamiento asociado a la actividad de los rifts.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT An extensive lake existed during part of the Oligocene and almost all the Miocene in the region located east of the southern end of the Sierra Madre Occidental (SMOc). The lake was formed in a tectonic depression associated with the Aguascalientes graben and the Teocaltiche half-graben. Sediments accumulated inside this continental basin are epiclastic, mainly derived from volcanic rocks of the SMOc, and from the volcanic cover of the Mesa Central, chemical and biochemical precipitates (fresh water limestone), and mixed sediments, as well as far less voluminous, but ubiquitous, volcanic ash-fall layers, which were used to obtain U-Pb ages from zircons. The age range of the basin-fill sediments is broad, varying from Rupelian (~28.6 Ma) to Tortonian (~7.6 Ma). Previously, on the basis of fossil fauna, the succession was considered only as late Miocene in age. The southern end of the SMOc includes several NNE-trending basins of tectonic origin that contained lakes. Based on the characteristics of the individual sedimentary successions, and on their fossil faunas, it is known that three of these basins (Tlaltenango, Juchipila and Teocaltiche) had lakes at the same time. The fourth basin, the Bolaños graben, located west and parallel to the Tlaltenango basin, probably also had a lake during the Neogene, but almost all its sediments have been eroded, so that little is known about them. In order to explain the simultaneous partial closure of all the drainage systems a common, regional, cause must be invoked. All the tectonic basins in the southern part of the SMOc end close to the tectonic depressions related to either the Tepic-Zacoalco or Tula-Chapala rifts. Isostatic uplift of the footwall blocks of these ~E-W-trending rifts may have provoked partial closure of hydrologic systems within the NNE-trending grabens. It is not known when the basins were opened and ceased to act as aggrading systems, but the apparent absence of Blancan age fossils within them may indicate that they could have been opened prior to ~4.75 Ma, which is the numerical value of the beginning of this faunal stage. A probable common cause for the simultaneous opening could be a marine invasion in the region now occupied by the Gulf of California. The new base level of erosion probably increased the stream gradients in the fluvial systems, providing enough energy to the axial rivers within the grabens to overcome the uplift associated with ~E-W rift activity.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[paleolago]]></kwd>
<kwd lng="es"><![CDATA[secuencia volcánica-sedimentaria]]></kwd>
<kwd lng="es"><![CDATA[edades U-Pb en circón]]></kwd>
<kwd lng="es"><![CDATA[paleocuenca Teocaltiche]]></kwd>
<kwd lng="es"><![CDATA[semigraben de Teocaltiche]]></kwd>
<kwd lng="es"><![CDATA[graben de Aguascalientes]]></kwd>
<kwd lng="es"><![CDATA[México]]></kwd>
<kwd lng="en"><![CDATA[paleo-lake]]></kwd>
<kwd lng="en"><![CDATA[volcanic-sedimentary sequence]]></kwd>
<kwd lng="en"><![CDATA[zircon U-Pb ages]]></kwd>
<kwd lng="en"><![CDATA[Teocaltiche paleo-basin]]></kwd>
<kwd lng="en"><![CDATA[Teocaltiche half-graben]]></kwd>
<kwd lng="en"><![CDATA[Aguascalientes graben]]></kwd>
<kwd lng="en"><![CDATA[Mexico]]></kwd>
</kwd-group>
</article-meta>
</front><back>
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