<?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>S1405-33222022000100109</article-id>
<article-id pub-id-type="doi">10.18268/bsgm2022v74n1a161021</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[Magnetic fabric and sedimentary characterization of near-slope to basinal deposits from the Chicontepec Formation, central and southern region of the Tampico-Misantla basin]]></article-title>
<article-title xml:lang="es"><![CDATA[Fábrica magnética y caracterización de depósitos sedimentarios cercanos a la cuenca de la Formación Chicontepec, región centro y sur de la cuenca Tampico-Misantla]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Molina-Garza]]></surname>
<given-names><![CDATA[Roberto Stanley]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Sierra-Rojas]]></surname>
<given-names><![CDATA[María Isabel]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad Nacional Autónoma de México Centro de Geociencias ]]></institution>
<addr-line><![CDATA[ Querétaro]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad de los Andes Departamento de Geociencias ]]></institution>
<addr-line><![CDATA[ Bogotá D.C.]]></addr-line>
<country>Colombia</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>00</month>
<year>2022</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>00</month>
<year>2022</year>
</pub-date>
<volume>74</volume>
<numero>1</numero>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1405-33222022000100109&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1405-33222022000100109&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1405-33222022000100109&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT We report results of a study of the Chicontepec Formation magnetic fabric in the central and southern region of the Tampico-Misantla basin in the state border region between Veracruz and Hidalgo. Samples were collected at 16 sites corresponding to two main facies associations: channel-fill facies and channel overbank facies. The channel facies dominate the relief developing prominent geoforms adjacent to low hills developed in facies dominated by shales. Measurements were made on channel and overbank facies. Laboratory analyses include anisotropy of magnetic susceptibility (AMS) and remanence anisotropy (AARM), as well as isothermal remanence acquisition (IRM) and thermomagnetic curves to characterize magnetic mineralogy. The magnetic susceptibility values of the entire collection are of the order of 40 to 70 x10-6 SI, so the susceptibility fabric is controlled by the paramagnetic fraction. The IRM acquisition curves are near saturation with inductions &lt; 0.3 T and can be modeled with a low coercivity component contributing ~ 90% and a high coercivity component contributing &lt; 10%. The thermomagnetic curves are dominated by paramagnetic phases. In the AMS fabric, three types of behavior are observed, corresponding to a lesser extent to sedimentary fabrics (k3 ~ vertical), and mostly to incipient and well-developed tectonic fabrics. The sedimentary fabrics are characterized by the imbrication of the magnetic foliation perpendicular to the paleocurrent data obtained in the field, which are generally consistent from NW to SE. At sites with tectonic fabric, which generally correspond to sites closer to the deformation front, the magnetic lineaments are well clustered in the NW quadrant with low plunges. AMS and AARM fabrics may combine in complex patterns. AARM appears to record either maximum axis directions that correspond to alignment of elongated particles perpendicular to flow or the direction of thrust motion.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN Presentamos los resultados de un estudio de la fábrica magnética de la Formación Chicontepec en la región central y sur de la cuenca TampicoMisantla cerca del límite estatal entre Veracruz e Hidalgo. Se recolectaron muestras en 16 sitios correspondientes a dos asociaciones de facies principales: facies de relleno de canal y facies de desborde de canal. Las facies del canal dominan el relieve desarrollando geoformas prominentes adyacentes a colinas bajas desarrolladas en facies dominadas por lutitas. Se realizaron mediciones en facies de canal y de desborde de canal. Los análisis de laboratorio incluyen anisotropía de susceptibilidad magnética (AMS) y anisotropía de remanencia (AARM), así como adquisición de remanencia isotérmica (IRM) y curvas termomagnéticas para caracterizar la mineralogía magnética. Los valores de susceptibilidad magnética son del orden de 40 a 70 x 10-6 SI, por lo que la fábrica de susceptibilidad está controlada por la fracción paramagnética. Las curvas de adquisición de IRM están cerca de la saturación con inducciones &lt; 0.3 T y se pueden modelar con un componente de baja coercitividad que contribuye con ~ 90% y un componente de alta coercitividad que contribuye con &lt; 10%. Las curvas termomagnéticas están dominadas por fases paramagnéticas. En la fábrica AMS se observan tres tipos de comportamiento, correspondientes en menor medida a fábricas sedimentarias (k3 ~ vertical), y sobre todo a fábricas tectónicas que van de incipientes a bien desarrolladas. Las fábricas tectónicas se caracterizan por la imbricación de la foliación magnética perpendicular a los datos de paleocorriente obtenidos en campo, que generalmente son consistentes de NW a SE. Los sitios con fábrica tectónica generalmente corresponden a sitios cercanos al frente de deformación o de niveles estructurales profundos. Las lineaciones magnéticas de varios sitios están bien agrupadas en el cuadrante SW en la dirección de movimiento en las cabalgaduras.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[magnetic fabric]]></kwd>
<kwd lng="en"><![CDATA[Chicontepec Formation]]></kwd>
<kwd lng="en"><![CDATA[turbidite systems]]></kwd>
<kwd lng="es"><![CDATA[fábrica magnética]]></kwd>
<kwd lng="es"><![CDATA[Formación Chicontepec]]></kwd>
<kwd lng="es"><![CDATA[sistemas turbidíticos]]></kwd>
</kwd-group>
</article-meta>
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