<?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>S1026-87742016000100049</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Geodinámica de la subcuenca Lomas de Olmedo, noroeste argentino, interpretada a partir de un modelo de compensación local y del análisis estadístico de datos gravimétricos]]></article-title>
<article-title xml:lang="en"><![CDATA[Geodynamics of the Lomas de Olmedo subbasin, northeastern Argentina, interpreted from a local compensation model and statistical analysis of gravimetric data]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Antonio García]]></surname>
<given-names><![CDATA[Héctor Pedro]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
<xref ref-type="aff" rid="Aaf"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Lince Klinger]]></surname>
<given-names><![CDATA[Federico]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
<xref ref-type="aff" rid="Aaf"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Giménez]]></surname>
<given-names><![CDATA[Mario Ernesto]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
<xref ref-type="aff" rid="Aaf"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Ruiz]]></surname>
<given-names><![CDATA[Francisco]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Consejo Nacional de Investigaciones Científicas y Técnicas  ]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
<country>Argentina</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad Nacional de San Juan Facultad de Ciencias Exactas, Físicas y Naturales ]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
<country>Argentina</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>04</month>
<year>2016</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>04</month>
<year>2016</year>
</pub-date>
<volume>33</volume>
<numero>1</numero>
<fpage>49</fpage>
<lpage>58</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1026-87742016000100049&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1026-87742016000100049&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1026-87742016000100049&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN La subcuenca Lomas de Olmedo es uno de los depocentros que conforman la gran cuenca cretácica-paleógena del noroeste de Argentina, formando parte de la inmensa llanura Chaco-Bonaerense, con un rumbo dominante suroeste-nordeste. Se trata de una típica cuenca de rift continental en el sentido de "punto de unión triple". Se evaluó el estado isostático en que se encuentra el depocentro Lomas de Olmedo a partir de la consideración de un modelo de compensación de Airy-Heiskanen y mediante el análisis estadístico de las anomalías gravimétricas. Se obtuvo para la región en estudio una carta del Moho hidrostático bajo la hipótesis de Airy-Heiskanen, la cual considera tanto la raíz que compensa la carga topográfica, como la anti-raíz del depocentro Lomas de Olmedo, el cual presenta una espesa columna sedimentaria cercana a los 6 kilómetros. Además, se calculó la anomalía isostática local, afectando a la anomalía de Bouguer Completa por la corrección geológica o corrección por sedimentos y posteriormente por el efecto gravimétrico del Moho hidrostático. Se identificó una anomalía isostática negativa que cubre prácticamente toda la extensión de la subcuenca Lomas de Olmedo. De acuerdo a este modelo de compensación para el depocentro, esta anomalía podría indicar un estado de subcompensación de la subcuenca, es decir, una carencia de anti-raíz. Este estado de subcompensación de la subcuenca Lomas de Olmedo, también fue interpretado al evaluar las regresiones estadísticas de las anomalías de Bouguer Completas versus altitudes topográficas.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT The Lomas the Olmedo trough is located within the Chaco-Bonaerense plain. It has a southwest-northeast trend and is one of the depocenters of the cretaceous-paleogene basin (northwestern Argentina). This trough is a typical continental rift basin in the sense of "triple junction point". The isostatic state of Lomas the Olmedo trough was evaluated through the Airy-Heiskanen's isostatic compensation model and the statistical analysis of the gravity anomalies. The Airy-Heiskanen model was used to derive an hydrostatic Moho map of the study area. This hydrostatic Moho includes the root that compensates topography and the anti-root from Lomas the Olmedo trough, which hosts a thick sedimentary column of nearly 6 kilometers. Additionally, the local isostatic anomaly was calculated. It was made, affecting the Complete Bouguer anomaly by a geological correction or correction for sediment and then by the gravimetric effect of the hydrostatic Moho. An extensive negative isostatic anomaly covering most of Lomas the Olmedo trough was identified. According this compensation model for the depocenter, this anomaly may indicate that the depocenter is isostatically sub-compensated or that there is a deficit of anti-root. The sub-compensation state was also observed through statistical regressions between Complete Bouguer anomalies and topographic altitudes.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[Gravimetría]]></kwd>
<kwd lng="es"><![CDATA[isostasia]]></kwd>
<kwd lng="es"><![CDATA[subcuenca Lomas de Olmedo]]></kwd>
<kwd lng="es"><![CDATA[geodinámica]]></kwd>
<kwd lng="en"><![CDATA[gravimetry]]></kwd>
<kwd lng="en"><![CDATA[isostasy]]></kwd>
<kwd lng="en"><![CDATA[Lomas the Olmedo trough]]></kwd>
<kwd lng="en"><![CDATA[Geodynamics]]></kwd>
</kwd-group>
</article-meta>
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