<?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>2007-8196</journal-id>
<journal-title><![CDATA[Epistemus (Sonora)]]></journal-title>
<abbrev-journal-title><![CDATA[Epistemus (Sonora)]]></abbrev-journal-title>
<issn>2007-8196</issn>
<publisher>
<publisher-name><![CDATA[Universidad de Sonora, División de Ingeniería]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S2007-81962021000200031</article-id>
<article-id pub-id-type="doi">10.36790/epistemus.v15i31.188</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Firmas de ree en intrusivos asociados a pórfidos de cobre en Sonora]]></article-title>
<article-title xml:lang="en"><![CDATA[Ree signatures of intrusives associated with porphyry copper of Sonora]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Santillana-Villa]]></surname>
<given-names><![CDATA[Cecilia]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Valencia-Moreno]]></surname>
<given-names><![CDATA[Martín]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Ochoa-Landín]]></surname>
<given-names><![CDATA[Lucas]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Del Río-Salas]]></surname>
<given-names><![CDATA[Rafael]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad Nacional Autónoma de México Instituto de Geología Estación Regional del Noroeste]]></institution>
<addr-line><![CDATA[Hermosillo Sonora]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad Nacional Autónoma de México Instituto de Geología Estación Regional del Noroeste]]></institution>
<addr-line><![CDATA[Hermosillo Sonora]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Universidad de Sonora Departamento de Geología ]]></institution>
<addr-line><![CDATA[Hermosillo Sonora]]></addr-line>
<country>Mexico</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>12</month>
<year>2021</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>12</month>
<year>2021</year>
</pub-date>
<volume>15</volume>
<numero>31</numero>
<fpage>31</fpage>
<lpage>37</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S2007-81962021000200031&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S2007-81962021000200031&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S2007-81962021000200031&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen Las firmas de REE en muestras de rocas plutónicas de cinco sistemas de pórfido de cobre en Sonora, sugieren que existe un proceso petrogenético a partir del enfriamiento de un plutón principal que genera columnas de magma de textura porfídica, emplazada en niveles más someros de la corteza. Esto es revelado por una aparente inversión en la polaridad de la anomalía de europio en los patrones normalizados de REE. En general, los patrones muestran una pendiente enriquecida en LREE, con una anomalía negativa de europio bien desarrollada en el caso del plutón principal. Las firmas de los intrusivos asociados con la mineralización son muy similares, a excepción de que la anomalía de europio se hace menos negativa e incluso positiva. De acuerdo con los modelos existentes, esto puede explicarse considerando que hay un fraccionamiento importante de hornblenda durante la generación del stock porfídico, tal vez en condiciones magmáticas más reductoras.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract REE signatures in samples of plutonic rocks from five copper porphyry systems in Sonora, suggest that there is a petrogenetic process linked to the cooling of a major pluton that generates magma columns of porphyritic texture, which are emplaced at shallow levels in the crust. This is revealed by an apparent reversal in the polarity of the europium anomaly in the REE normalized patterns. In general, the patterns display a LREE-enriched slope, with a well-developed negative europium anomaly in the case of the main pluton. The signatures of the intrusives associated with mineralization are very similar, excepting the europium anomaly, which becomes less negative and even positive. According to existing models, this can be explained by considering that there is a significant fractionation of hornblende during the generation of the porphyritic stock, perhaps under more reducing magmatic conditions.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[pórfidos de cobre]]></kwd>
<kwd lng="es"><![CDATA[REE]]></kwd>
<kwd lng="es"><![CDATA[anomalía de europio]]></kwd>
<kwd lng="en"><![CDATA[Copper porphyry]]></kwd>
<kwd lng="en"><![CDATA[REE]]></kwd>
<kwd lng="en"><![CDATA[europium anomaly]]></kwd>
</kwd-group>
</article-meta>
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