<?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>S1026-87742018000100018</article-id>
<article-id pub-id-type="doi">10.22201/cgeo.20072902e.2018.1.534</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Caverna del Valle de Los Lisos: una hipótesis sobre su origen en el contexto geomorfológico de las Sierras de Córdoba, Argentina]]></article-title>
<article-title xml:lang="en"><![CDATA[Cavern of El Valle de Los Lisos: a hypothesis about its origin in the geomorphological context of the Sierras de Córdoba]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[García-Aráoz]]></surname>
<given-names><![CDATA[Eduardo]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Madelón]]></surname>
<given-names><![CDATA[Nicolás]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Cioccale]]></surname>
<given-names><![CDATA[Marcela]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad Nacional de Córdoba  ]]></institution>
<addr-line><![CDATA[Córdoba Córdoba]]></addr-line>
<country>Argentina</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Córdoba  ]]></institution>
<addr-line><![CDATA[Córdoba Córdoba]]></addr-line>
<country>Argentina</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Universidad Nacional de Córdoba  ]]></institution>
<addr-line><![CDATA[Córdoba Córdoba]]></addr-line>
<country>Argentina</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>00</month>
<year>2018</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>00</month>
<year>2018</year>
</pub-date>
<volume>35</volume>
<numero>1</numero>
<fpage>18</fpage>
<lpage>27</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1026-87742018000100018&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1026-87742018000100018&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1026-87742018000100018&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen: La caverna del Valle de Los Lisos conforma el cierre de una cuenca hidrográfica de aproximadamente 133 hectáreas, ubicada en el macizo Los Gigantes del batolito de Achala, en la Provincia de Córdoba, en la parte central de Argentina. Se compone de una serie de intrincados pasadizos desarrollados en litología granítica, con 20 metros de avance horizontal en sentido Norte-Sur y 25 metros de descenso total. Por su nivel inferior circula el arroyo que drena la cuenca. De acuerdo con las observaciones realizadas, se propone un modelo genético-evolutivo de la caverna que es consistente con la evolución geomorfológica regional de las Sierras de Córdoba, y consta de tres etapas luego del emplazamiento del cuerpo intrusivo: 1) Desarrollo de un perfil de meteorización profundo que condiciona la formación de un paleo-relieve con predominio de una morfología abochonada. 2) A partir de un escarpe mixto (erosivo y estructural), la generación de la cuenca hidrográfica que alimenta el cauce que circula a través de la caverna. 3) Formación de las galerías principales en sucesivas fases de erosión.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract: The cavern of El Valle de Los Lisos is the closure of a watershed of approximately 133 hectares, located in Los Gigantes massif of the Achala batholith, Córdoba province, Argentina. This cavern is formed by a set of intricated passages developed in a granitic rock. The passages have 20 meters of horizontal advance in North-South direction, and 25 meters of total descent. The stream that drains the basin flows through its lower level. According to the observations, a genetic-evolutionary model of the cavern is proposed, which is consistent with the Sierras de Córdoba regional geomorphological evolution. The model consists of three stages after the emplacement of intrusive body: 1) A deep weathering profile development that conditions the formation of a paleo-relief with a predominance of a rounded morphology; 2) Hydrographic basin generation from an erosive and structural escarpment, which feeds the channel that circulates through the cave; 3) Main galleries formation in successive erosion phases.]]></p></abstract>
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<kwd lng="es"><![CDATA[cueva]]></kwd>
<kwd lng="en"><![CDATA[speleology]]></kwd>
<kwd lng="en"><![CDATA[granitic rocks]]></kwd>
<kwd lng="en"><![CDATA[landforms]]></kwd>
<kwd lng="en"><![CDATA[cave]]></kwd>
</kwd-group>
</article-meta>
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