<?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>S1405-33222017000200447</article-id>
<article-id pub-id-type="doi">10.18268/bsgm2017v69n2a9</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Variación en la composición isotópica del agua meteórica a lo largo de la sección centro-noreste de la Sierra Madre Oriental]]></article-title>
<article-title xml:lang="en"><![CDATA[Variation in isotopic composition of meteoric water along the central-northeastern section of the Mexican Fold-and-Thrust Belt, Sierra Madre Oriental]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Aguilar-Ramírez]]></surname>
<given-names><![CDATA[César F.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Camprubí]]></surname>
<given-names><![CDATA[Antoni]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Fitz-Díaz]]></surname>
<given-names><![CDATA[Elisa]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Cienfuegos-Alvarado]]></surname>
<given-names><![CDATA[Edith]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Morales-Puente]]></surname>
<given-names><![CDATA[Pedro]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad Nacional Autónoma de México Programa de Posgrado en Ciencias de la Tierra ]]></institution>
<addr-line><![CDATA[CDMX ]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad Nacional Autónoma de México Instituto de Geología ]]></institution>
<addr-line><![CDATA[CDMX ]]></addr-line>
<country>Mexico</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>00</month>
<year>2017</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>00</month>
<year>2017</year>
</pub-date>
<volume>69</volume>
<numero>2</numero>
<fpage>447</fpage>
<lpage>463</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1405-33222017000200447&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1405-33222017000200447&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1405-33222017000200447&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN Se analizan las variaciones en la composición isotópica de agua meteórica a lo largo de una sección en el Cinturón de Pliegues y Cabalgaduras Mexicano, ubicado en la sección centro-noreste de la Sierra Madre Oriental. El objetivo de ello es determinar dichas variaciones en función de:1) el incremento en la elevación topográfica y 2) la distancia de las precipitaciones al interior del continente, desde que se produjo la evaporación de agua oceánica del Golfo de México. Se consideraron las características topográficas y climáticas de la sección estudiada, seleccionada por presentar las ventajas detalladas como sigue. La deformación en esta sección generó un rasgo de cuña orogénica, que le confiere una pendiente promedio entre 1º y 1.5º, sin la presencia de barreras topográficas que dificulten la libre circulación de vientos. Ello favorece evaluar variaciones significativas en la composición isotópica de H y O en función de la elevación topográfica. La sección se ubica a una latitud prácticamente constante entre 21º y 22º N, y la temperatura media anual decrece gradualmente desde el antepaís hacia el transpaís de la sección durante los periodos de precipitación. El muestreo de agua meteórica se efectuó mediante la colocación de 12 colectores de agua de lluvia en lugares elevados, a alturas entre 2740 y 56 msnm a lo largo de la sección estudiada. Asimismo, se tomaron muestras de agua de ríos y manantiales durante la temporada de lluvia de 2012 en zonas de escorrentía constante, de 7 localidades diferentes. Los valores obtenidos en agua de lluvia varían entre -4.89 y -11.75 &#8240; para &#948;18O y entre -25.35 y -80.34 &#8240; para &#948;2H (respecto a VSMOW). Así, se determinó una Línea de Agua Meteórica local (LAML) definida por la ecuación &#948;2H = &#948;18O * 8.15 + 15. La tasa de fraccionamiento obtenida para O y H (&#948;18O y &#948;2H) respecto a la elevación, fue de 2.19 &#8240; km-1 y 17.75 &#8240; km-1, respectivamente. La LAML y las tasas de fraccionamiento obtenidos en este estudio podrán ser utilizados como valores de referencia a nivel regional para evaluar el papel del agua meteórica involucrada en procesos atmosféricos y corticales superficiales.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT We analyze the variations in isotopic composition of meteoric water along a transect in the Mexican Fold-Thrust Belt, located in the central-northeastern part of the Sierra Madre Oriental. The aim is to determine such variations as a function of 1) increasing topographic elevation and 2) the distance of rain inside the continent since evaporation occurrence of oceanic water from the Gulf of Mexico. Topographic and climate characteristics were considered in the studied section, which was chosen because it presents some advantages as follows. Deformation in this section exhibits orogenic wedge features, which generated an average slope between 1° and 1.5°, with no topographic barriers that obstruct the free circulation of wind. This allows us to evaluate significant isotopic variations of H and O as a function of topographic elevation. The section is located at constant latitude between 21° and 22° N. Furthermore, the average annual temperature decreases gradually from the foreland to the hinterland of the section during precipitationperiods. Sampling of meteoric water wascarried out by installing 12 rainwater collectors at heights between 2740 and 56 masl along the transect. Additionally, water samples were collected in rivers and springs during the 2012 rain season in zones of constant water runoff in 7 different localities. Obtained values from rain water vary between -4.89 and -11.75% for &#948;18O and between -25.35 and -80.34 &#8240; for &#948;2H (relative to VSMOW)- These allowed to determine a Local Meteoric WaterLine (LMWL) defined by the equation &#948;2H = &#948;18O * 8.15 + 15. With this, fractionation rate relative to elevation for O and H (&#948;18O y &#948;2H) were obtained at 2.19 &#8240; km-1 and 17.75 &#8240; km-1, respectively. The LMWL and fractionation rates obtained in this study can be used as regional-scale references in order to evaluate the role of meteoric water involved in atmospheric and shallow cortical processes.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[Composición isotópica]]></kwd>
<kwd lng="es"><![CDATA[&#948;2H]]></kwd>
<kwd lng="es"><![CDATA[&#948;18O]]></kwd>
<kwd lng="es"><![CDATA[agua meteórica]]></kwd>
<kwd lng="es"><![CDATA[fraccionamiento isotópico]]></kwd>
<kwd lng="es"><![CDATA[isótopos estables]]></kwd>
<kwd lng="en"><![CDATA[Isotopic composition]]></kwd>
<kwd lng="en"><![CDATA[&#948;2H]]></kwd>
<kwd lng="en"><![CDATA[&#948;18O]]></kwd>
<kwd lng="en"><![CDATA[meteoric water]]></kwd>
<kwd lng="en"><![CDATA[isotopic fractionation]]></kwd>
<kwd lng="en"><![CDATA[stable isotopes]]></kwd>
</kwd-group>
</article-meta>
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