<?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>S1026-87742023000300227</article-id>
<article-id pub-id-type="doi">10.22201/cgeo.20072902e.2023.3.1739</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Estudio litosférico del Margen Continental Argentino: comportamiento isostático y derivaciones tectónicas]]></article-title>
<article-title xml:lang="en"><![CDATA[Lithospheric study of the Argentine Continental Margin: isostatic behavior, and tectonic implications]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Pizarro]]></surname>
<given-names><![CDATA[Guillermo Domingo]]></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 contrib-type="author">
<name>
<surname><![CDATA[Arecco]]></surname>
<given-names><![CDATA[María Alejandra]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
<xref ref-type="aff" rid="Aaf"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Ghidella]]></surname>
<given-names><![CDATA[Marta]]></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 Instituto Geofísico-Sismológico Ing. F. Volponi]]></institution>
<addr-line><![CDATA[Rivadavia San Juan]]></addr-line>
<country>Argentina</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad Nacional de San Juan Facultad de Ciencias Exactas, Físicas y Naturales Departamento de Biología]]></institution>
<addr-line><![CDATA[Rivadavia San Juan]]></addr-line>
<country>Argentina</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Universidad de Buenos Aires Facultad de Ingeniería Instituto de Geodesia y Geofísica Aplicadas]]></institution>
<addr-line><![CDATA[Buenos Aires ]]></addr-line>
<country>Argentina</country>
</aff>
<aff id="Af4">
<institution><![CDATA[,Universidad de la Defensa Nacional Facultad de la Armada Escuela de Ciencias del Mar]]></institution>
<addr-line><![CDATA[Buenos Aires ]]></addr-line>
<country>Argentina</country>
</aff>
<aff id="Af5">
<institution><![CDATA[,Ministerio de Relaciones Exteriores, Comercio Internacional y Culto Cancillería Argentina Instituto Antártico Argentino]]></institution>
<addr-line><![CDATA[Buenos Aires ]]></addr-line>
<country>Argentina</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>00</month>
<year>2023</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>00</month>
<year>2023</year>
</pub-date>
<volume>40</volume>
<numero>3</numero>
<fpage>227</fpage>
<lpage>240</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1026-87742023000300227&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1026-87742023000300227&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1026-87742023000300227&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN El presente trabajo es un estudio de la litosfera continental y oceánica en el Margen Continental Argentino. Estas investigaciones están basadas en datos geofísicos existentes en la zona correspondiente a la plataforma, talud, emersión y llanura abisal de Argentina, comprendida entre los 50° a 66° de longitud oeste y 36° a 50° de latitud sur. El mismo consiste en la obtención de un modelo de compensación isostática de la zona y su correlación con modelos existentes. Con el doble objetivo de evaluar el com portamiento isostático de la región y buscar mecanismos que permitan explicar su desarrollo, se consideran modelos de compensación local (mecanismo de Airy) y compensación regional (mecanismo Flexural). Siendo correlacionados con los modelos de a) Profundidad del Basamento y Espesores Sedimentarios, b) Profundidad de la Discontinuidad corteza-manto superior y c) Profundidad del Punto de Curie (CPD, Curie Point Depth), para analizar el estado isostático de la zona de cuencas offshore, adelgazamiento cortical y niveles astenosféricos, entre otras cosas. El análisis comparativo de estos elementos permite determinar el grado de compensación isostática de esta zona, la geometría de las cuencas offshore en su relación con el adelgazamiento cortical y ascenso astenosférico, ubicar los sectores donde el manto superior estaría magnetizado, modelar la asimetría lístrica de la cuenca del Colorado, determinar por primera vez los límites y geometría de los altos estructurales de Belén y San Javier y discutir las causas que dan origen a la gran profundidad del basamento en la Cuenca Argentina, entre otras como zonas de sepentinización y la zona de falla de transformación de Belén. De la misma manera se abren interrogantes que requieren nuevos análisis y estudios, como los relacionados al CPD en las cuencas de Valdés, sectorizar la zona modelada para buscar un mejor ajuste de densidades, profundizar las causas de la gran batimetría de la Cuenca Argentina, entre otros.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT This work is a study of the continental and oceanic lithosphere in the Argentine Continental Margin. These investigations are based on existing geophysical data in the area corresponding to the platform, slope, emersion and abyssal plain of Argentina, between 50° to 66° west longitude and 36° to 50° south latitude. It consists of obtaining a model of isostatic compensation of the area and its correlation with existing models. With the dual objective of evaluating the isostatic behavior of the region and searching for mechanisms to explain its development, models of local compensation (Airy mechanism) and regional compensation (flexural mechanism) are considered. In this study we use the models of a) Sedimentary Thickness and Basement Depth, b) Depth of the upper crust-mantle discontinuity and c) Curie Point Depth (CPD) in order to analyse the isostatic state of the offshore basin zone, crustal thinning and asthenospheric levels, among other things. The correlation of these elements allows to determine the degree of isostatic compensation in this zone, geometry of the offshore basins in relation to crustal thinning and asthenospheric ascent, locate the sectors where the upper mantle would be magnetized, model the listric asymmetry of the Colorado basin, determine for the first time the limits and geometry of the structural highs of Belén and San Javier and discuss the causes that give rise to the great depth of the basement in the Argentine Basin, among others like serpentinization zones and Belen transform zone. In the same way, questions arise that require new analyses and studies, such as those related to the CPD in the Valdés basins, sectorize the modelled area to seek a better density adjustment, deepen the causes of the great bathymetry of the Argentine Basin, among others.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[descompensación isostática]]></kwd>
<kwd lng="es"><![CDATA[cuencas offshore]]></kwd>
<kwd lng="es"><![CDATA[Profundidad del Punto de Curie]]></kwd>
<kwd lng="es"><![CDATA[Moho gravimétrico]]></kwd>
<kwd lng="en"><![CDATA[isostatic decompensation]]></kwd>
<kwd lng="en"><![CDATA[offshore basins]]></kwd>
<kwd lng="en"><![CDATA[Curie Point Depth]]></kwd>
<kwd lng="en"><![CDATA[gravimetric Moho]]></kwd>
</kwd-group>
</article-meta>
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