<?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>0016-7169</journal-id>
<journal-title><![CDATA[Geofísica internacional]]></journal-title>
<abbrev-journal-title><![CDATA[Geofís. Intl]]></abbrev-journal-title>
<issn>0016-7169</issn>
<publisher>
<publisher-name><![CDATA[Universidad Nacional Autónoma de México, Instituto de Geofísica]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S0016-71692024000401147</article-id>
<article-id pub-id-type="doi">10.22201/igeof.2954436xe.2024.63.4.1780</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Nuevas observaciones en la corteza continental transicional del sur del Golfo de México y sus implicaciones en los modelos de margen continental]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Rodríguez]]></surname>
<given-names><![CDATA[Joel Rosales]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Instituto Mexicano del Petróleo Dirección de Investigación ]]></institution>
<addr-line><![CDATA[ CDMX]]></addr-line>
<country>México</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Instituto Politécnico Nacional Escuela Superior de Ingeniería y Arquitectura ]]></institution>
<addr-line><![CDATA[ CDMX]]></addr-line>
<country>México</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>12</month>
<year>2024</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>12</month>
<year>2024</year>
</pub-date>
<volume>63</volume>
<numero>4</numero>
<fpage>1147</fpage>
<lpage>1164</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S0016-71692024000401147&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S0016-71692024000401147&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S0016-71692024000401147&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen La interpretación de las propiedades físicas de la corteza y manto comúnmente se hace a partir de la asociación de velocidades sísmicas con la mineralogía de las rocas ígneas que las constituyen, dado que los afloramientos de corteza o manto exhumados o pozos que cortan las rocas de basamento continental u oceánico son escasos. La corteza oceánica del Golfo de México se caracteriza por velocidades sísmicas de 6.1-6.9 km/s, asociadas a gabros. Se observan diferencias en el rango de velocidades sísmicas entre la porción oriental y occidental de la corteza oceánica, tanto a nivel de corteza como en el manto. Se identifican anomalías de velocidades sísmicas entre la corteza y el manto, principalmente en áreas cercanas al límite corteza oceánica-continental. Estas anomalías de velocidades sísmicas se asocian a intrusiones máficas ocurridas durante la apertura del Golfo de México. Estas intrusiones también se interpretan en la base de la corteza a partir del modelado magnético de un perfil en el sur del Golfo de México. Con el modelado magnético se interpreta manto serpentinizado en el área de la Anomalía Magnética de Campeche. Con ambas interpretaciones se sugieren dos periodos de evolución tectónica del Golfo de México; el primer periodo es asociado a un margen continental no volcánico, en el cual ocurre la exhumación y la serpentinización del manto, el segundo periodo asociado a un margen volcánico en el cual ocurre la intrusión de rocas máficas cercanas al límite corteza oceánica-continental y la rotación de Yucatán.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract The interpretation of physical properties of crust and mantle is commonly done from the relationship between seismic velocities with mineralogy of igneous rocks that constitute them, mainly due to scarce outcrops of exhumed crust or mantle, and wells that cut continental or oceanic basement. The oceanic crust of the Gulf of Mexico is characterized by seismic velocities of 6.1-6.9 km/s, associated with gabbro. Differences in the range of seismic velocities are observed, between the eastern and western portion of the crust, both at the crustal and mantle level. In areas close to the oceanic-continental crust boundary, anomalies of seismic velocities are distinguished overlying the mantle, associated with mafic intrusions occurred during the Gulf of Mexico opening. These intrusions are also interpreted at the base of continental crust from the magnetic modeling 2D in the southern Gulf of Mexico. Over this profile serpentinized mantle is interpreted around Campeche Magnetic Anomaly. Two periods of tectonic evolution of the Gulf of Mexico are interpreted, the first one is associated with a non-volcanic continental margin, in which exhumation and serpentinization of the mantle occur, the second period is associated with a volcanic continental margin, the intrusion of mafic rocks occurs, mainly close to the oceanic-continental crust boundary, and the Yucatan rotation also occurs.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[Velocidad sísmica]]></kwd>
<kwd lng="es"><![CDATA[corteza oceánica]]></kwd>
<kwd lng="es"><![CDATA[serpentinización]]></kwd>
<kwd lng="es"><![CDATA[intrusión]]></kwd>
<kwd lng="es"><![CDATA[margen continenta]]></kwd>
<kwd lng="en"><![CDATA[Seismic velocity]]></kwd>
<kwd lng="en"><![CDATA[oceanic crust]]></kwd>
<kwd lng="en"><![CDATA[serpentinite]]></kwd>
<kwd lng="en"><![CDATA[intrusion]]></kwd>
<kwd lng="en"><![CDATA[continental margin]]></kwd>
</kwd-group>
</article-meta>
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</nlm-citation>
</ref>
<ref id="B126">
<nlm-citation citation-type="book">
<person-group person-group-type="author">
<name>
<surname><![CDATA[Zinecker]]></surname>
<given-names><![CDATA[M. P.]]></given-names>
</name>
</person-group>
<source><![CDATA[Structural and Stratigraphic Evolution of Three Mesozoic, Rifted-Passive Margins: Guinea Plateau, Demerara Rise, and the Southeastern Gulf of Mexico]]></source>
<year>2020</year>
<publisher-name><![CDATA[University of Houston]]></publisher-name>
</nlm-citation>
</ref>
</ref-list>
</back>
</article>
