<?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>S1405-33222020000100110</article-id>
<article-id pub-id-type="doi">10.18268/bsgm2020v72n1a111019</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Análisis morfométrico y morfotectónico de dos cuencas fluviales intermontanas colineales y opuestas de la Precordillera, Andes Centrales de Argentina]]></article-title>
<article-title xml:lang="en"><![CDATA[Morphometric and morphotectonic analysis of two collinear and opposite intermountain river basins in the Precordillera, Central Andes of Argentina]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Vargas]]></surname>
<given-names><![CDATA[Mariana]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Rothis]]></surname>
<given-names><![CDATA[Martin]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
<xref ref-type="aff" rid="Aaf"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Esper Angillieri]]></surname>
<given-names><![CDATA[Maria Yanina]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Perucca]]></surname>
<given-names><![CDATA[Laura]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
<xref ref-type="aff" rid="Aaf"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Vargas]]></surname>
<given-names><![CDATA[Nicolás]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad Nacional de San Juan Facultad de Ciencias Exactas, Físicas y Naturales ]]></institution>
<addr-line><![CDATA[San Juan ]]></addr-line>
<country>Argentina</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,UNSJ  ]]></institution>
<addr-line><![CDATA[San Juan ]]></addr-line>
<country>Argentina</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>00</month>
<year>2020</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>00</month>
<year>2020</year>
</pub-date>
<volume>72</volume>
<numero>1</numero>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1405-33222020000100110&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1405-33222020000100110&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1405-33222020000100110&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN Las cuencas fluviales Gualilán-La Cantera se localizan en el ámbito de Precordillera Central, Andes centro-occidentales de Argentina. El drenaje regional en esta depresión tectónica está controlado por el sistema de corrimientos que elevan la sierra de La Invernada por el oeste y por las fallas con actividad tectónica cuaternaria que constituyen el sistema de cabalgamiento La Cantera en su porción central y oriental. Ambas cuencas, colineales, opuestas, divergentes y con forma elongada en dirección N-S, se encuentran separadas por una suave divisora de aguas o portezuelo, sugiriendo que en el pasado constituyeron un mismo valle intermontano en el ámbito de Precordillera. El objetivo de este estudio es la caracterización morfométrica y morfotectónica de estas cuencas, complementada con un análisis de los procesos de captura fluvial. La cuenca del río Gualilán indicaría baja actividad tectónica cuaternaria de las estructuras que la limitan, mientras que las del río La Cantera poseen evidencia de mayor actividad tectónica cuaternaria. La pendiente media obtenida para la cuenca del río La Cantera es más elevada que la del río Gualilán. Además, el perfil del río Gualilán muestra knickpoints principalmente en su tramo superior. En cambio, el río La Cantera, además de mostrar knickpoints también en su tramo superior, posee los mayores quiebres de pendiente en su tramo inferior. El sistema de Falla La Cantera (en adelante SFLC) contribuiría a generar estas variaciones en la pendiente a lo largo de ambos ríos, producto del movimiento de esta estructura con actividad pleistocena tardía-holocena y probablemente histórica. También se identificó una falla inversa con componente horizontal y rumbo E-O, coincidente con la cabecera de ambos ríos principales N-S, que influiría en la dinámica de ambos colectores principales. El elevado gradiente del cauce principal N-S y el fuerte desnivel entre la cabecera y desembocadura del río La Cantera respecto del río Gualilán, son factores que favorecen directamente la mayor erosión observada en el primero en relación al segundo. Esta erosión es remontante y se ve además favorecida por desarrollarse en un ambiente de rocas fácilmente degradables (areniscas, limolitas y conglomerados del Neógeno). Se espera que la evolución del río La Cantera hacia el norte culminará en un futuro en un proceso de captura de la cuenca endorreica del río Gualilán y el desvío de sus caudales hacia el captor (hacia el sur), con la desembocadura en el río San Juan, que es el nivel de base de la región. Este proceso parece ser frecuente en numerosos valles tectónicos longitudinales de la Precordillera de San Juan, cuya causa de rejuvenecimiento es considerada en este trabajo como dinámica (tectónica).]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT The Gualilán and La Cantera river basins are located in the Central Precordillera of the central-western Andean ranges of Argentina. Both river basins lie in a N-S tectonic depression. The regional drainage in the depression is controlled by two thrust-fault systems. To the west lies a system of thrusts associated with the Invernada mountain range. The eastern area is controlled by the La Cantera thrust system. Both basins, collinear, opposite and divergent, with an elongated shape in the N-S direction, are separated by a smooth water divide or &#8220;portezuelo.&#8221; suggesting that in the past they comprised a single intermountain valley. The objective of this study is to make a morphometric and morphotectonic characterization of these river basins, complemented with an analysis of a stream piracy process. From this analysis, the Gualilán river basin suggests a low tectonic activity for the structures that cross the basin, while those of the La Cantera River have clear evidence of Quaternary tectonic activity. The average slope of the La Cantera river basin is steeper than that of the Gualilán river basin. Morover, the Gualilán longitudinal river profile shows several knickpoints, mainly in its upper section, while the La Cantera longitudinal river profile also shows knickpoints in its upper section but has the main slope breaks in its lower section. The La Cantera fault system would has contributed to generate these variations in the slope along both rivers, product of the late Pleistocene to Holocene and probably historical activity. This paper also describes a reverse fault with horizontal displacement trending E-W, coincident with the headwaters of both N-S rivers, which would also influence the dynamics of these basins. The high gradient of the main channel and the drop in elevation between the headwaters and the outlet of the La Cantera River with respect to the Gualilán River are factors that directly favor upstream erosion. Easily eroded rocks (sandstones, siltstones, and conglomerates of the Neogene) also favor the headward erosion. Erosion would culminate in a future process of piracy of the endorheic basin of the Gualilán River, and the deviation of its flows towards the captor (La Cantera River), down to the mouth of the San Juan River, which is the base level of the region. These capture processes seems to be frequent in many of the longitudinal tectonic valleys of the Precordillera, whose cause of rejuvenation is considered in this work as dynamic (tectonic).]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[Cuenca fluvial]]></kwd>
<kwd lng="es"><![CDATA[Captura fluvial]]></kwd>
<kwd lng="es"><![CDATA[Neotectónica]]></kwd>
<kwd lng="es"><![CDATA[Precordillera]]></kwd>
<kwd lng="en"><![CDATA[River basin]]></kwd>
<kwd lng="en"><![CDATA[Stream piracy]]></kwd>
<kwd lng="en"><![CDATA[Neotectonics]]></kwd>
<kwd lng="en"><![CDATA[Precordillera]]></kwd>
</kwd-group>
</article-meta>
</front><back>
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<page-range>83-108</page-range><publisher-loc><![CDATA[London, U.K. ]]></publisher-loc>
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<ref id="B50">
<nlm-citation citation-type="journal">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Zapata]]></surname>
<given-names><![CDATA[T.R.]]></given-names>
</name>
<name>
<surname><![CDATA[Allmendinger]]></surname>
<given-names><![CDATA[R.W.]]></given-names>
</name>
</person-group>
<article-title xml:lang=""><![CDATA[The thrust front zone of the Precordillera, Argentina: A Thick-skinned triangle zone]]></article-title>
<source><![CDATA[American Association of Petroleum Geologists Bulletin]]></source>
<year>1996</year>
<numero>80</numero>
<issue>80</issue>
<page-range>359-81</page-range></nlm-citation>
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</article>
