<?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>S1405-33222024000300007</article-id>
<article-id pub-id-type="doi">10.18268/bsgm2024v76n3a010324</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[Rock Magnetic and Geochemical Characterization of the Paleogene Carbonate Sequence in the Tekax Borehole, Yucatan, Mexico]]></article-title>
<article-title xml:lang="es"><![CDATA[Caracterización de roca magnética y geoquímica de la secuencia carbonatada del Paleógeno en el pozo Tekax, Yucatán, México]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Pérez-Cruz]]></surname>
<given-names><![CDATA[Ligia]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
<xref ref-type="aff" rid="Aaf"/>
<xref ref-type="aff" rid="A a"/>
<xref ref-type="aff" rid="A3"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Salomón-Dávila]]></surname>
<given-names><![CDATA[Daniel J.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
<xref ref-type="aff" rid="Aaf"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Vázquez-Sánchez]]></surname>
<given-names><![CDATA[Claudio]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
<xref ref-type="aff" rid="Aaf"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Ortega-Nieto]]></surname>
<given-names><![CDATA[Alejandro]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Escobar-Sánchez]]></surname>
<given-names><![CDATA[Elia J]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Valdés-Hernández]]></surname>
<given-names><![CDATA[Marysol]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
<xref ref-type="aff" rid="Aaf"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Venegas-Ferrer]]></surname>
<given-names><![CDATA[Rafael]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Urrutia-Fucugauchi]]></surname>
<given-names><![CDATA[Jaime]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
<xref ref-type="aff" rid="Aaf"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad Nacional Autónoma de México Instituto de Geofísica Programa Universitario de Perforaciones en Océanos y Continentes]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Instituto de Investigación Científica y Estudios Avanzados Chicxulub  ]]></institution>
<addr-line><![CDATA[Mérida Yucatán]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Universidad Nacional Autónoma de México Coordinación de la Investigación Científica Coordinación de Plataformas Oceanográficas]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af4">
<institution><![CDATA[,Universidad Nacional Autónoma de México Escuela Nacional de Estudios Superiores ]]></institution>
<addr-line><![CDATA[Mérida Yucatán]]></addr-line>
<country>Mexico</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>00</month>
<year>2024</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>00</month>
<year>2024</year>
</pub-date>
<volume>76</volume>
<numero>3</numero>
<fpage>0</fpage>
<lpage>0</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1405-33222024000300007&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1405-33222024000300007&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1405-33222024000300007&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT Formation of carbonates involve an interplay of processes, including climate, ocean circulation, marine organisms, sediment sources, transport, deposition and diagenesis. The Yucatan peninsula is characterized by a thick carbonate sequence, which has been studied by geological-geophysical surveys and drilling. Characterizing carbonate systems remains an important yet complex undertaking. Here, results of a magnetic susceptibility and X-ray fluorescence geo-chemical study are used to characterize the Paleogene carbonate sequence in the Tekax borehole of the Chicxulub Drilling Program. The carbonate sequence is ~222 m thick, formed by limestones, dolomites, carbonate breccias and evaporites. Changes in Si, Ca, Fe, Mg, Al, Ti and magnetic susceptibility correlate with lithology downcore. The Ca contents vary through the sequence with a trend around 24% and low discrete values. The upper unit shows higher Ca contents. The Si contents vary downhole, between about 0.03 to 38 %. The carbonates show weak magnetic susceptibilities associated with diamagnetic and paramagnetic minerals, characteristic of carbonate sediments and reduced terrigenous input. Magnetic hysteresis shows fine grained low coercivity magnetite and titanomagnetites, with PSD and MD domain states. Six units are identified through the lithological column. The carbonate sequence shows effects of varying dissolution, fracturing and dolomitization. The lower carbonate unit above the breccia contact shows evaporites, with gypsum and anhydrites.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN La formación de secuencias carbonatadas involucra diferentes factores, incluyendo) clima, circulación oceánica, organismos, fuentes de sedimentos, transporte, diagénesis y sedimentación. La península de Yucatán se caracteriza por secuencias de carbonatos, estudiadas en proyectos geológico-geofísicos y de perforaciones. La caracterización de carbonatos continúa presentando retos. En este estudio, se analizan los registros de susceptibilidad magnética y geoquímica de fluorescencia de rayos X de la secuencia Paleógena del pozo Tekax, Programa de Perforaciones Chicxulub. La secuencia Tekax está formada por calizas, dolomías, brechas carbonatadas y evaporitas. Los registros de Si, Ca, Fe, Mg, Al y Ti y de susceptibilidad magnética se correlacionan con la litología. El contenido de Ca varía con la profundidad, alrededor de un 24% con valores discretos bajos. La unidad superior muestra contenidos más altos. El contenido de Si varía entre 0.03 y 38%. La susceptibilidad magnética presenta valores bajos diamagnéticos y paramagnéticos, característicos de carbonatos con bajo aporte de terrígenos. Mediciones de histéresis a campos hasta 1.5 T indican minerales de baja coercitividad, posiblemente magnetita y titanomagnetitas con estados de dominio PSD y MD. Se identifican seis unidades en la sección del Paleógeno. La secuencia muestra efectos variables de disolución, fracturamiento y dolomitización. Los sedimentos basales arriba de las brechas de impacto muestran horizontes de evaporitas con yesos y anhidritas.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[Chicxulub crater]]></kwd>
<kwd lng="en"><![CDATA[Tekax borehole]]></kwd>
<kwd lng="en"><![CDATA[Yucatan peninsula]]></kwd>
<kwd lng="en"><![CDATA[Paleogene carbonate sequence]]></kwd>
<kwd lng="en"><![CDATA[Magnetic susceptibility]]></kwd>
<kwd lng="en"><![CDATA[X-ray fluorescence]]></kwd>
<kwd lng="es"><![CDATA[Cráter Chicxulub]]></kwd>
<kwd lng="es"><![CDATA[Pozo Tekax]]></kwd>
<kwd lng="es"><![CDATA[Península de Yucatán]]></kwd>
<kwd lng="es"><![CDATA[Secuencia carbonatada del Paleógeno]]></kwd>
<kwd lng="es"><![CDATA[Susceptibilidad Magnética]]></kwd>
<kwd lng="es"><![CDATA[Fluorescencia de rayos X]]></kwd>
</kwd-group>
</article-meta>
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