<?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>1026-8774</journal-id>
<journal-title><![CDATA[Revista mexicana de ciencias geológicas]]></journal-title>
<abbrev-journal-title><![CDATA[Rev. mex. cienc. geol]]></abbrev-journal-title>
<issn>1026-8774</issn>
<publisher>
<publisher-name><![CDATA[Universidad Nacional Autónoma de México, Instituto de Geología]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S1026-87742005000300345</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Marco geológico del pórfido de molibdeno El Crestón, Sonora central, México]]></article-title>
<article-title xml:lang="en"><![CDATA[Geological frame of the El Crestón molybdenum porphyry, central Sonora, Mexico]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Valenzuela-Navarro]]></surname>
<given-names><![CDATA[Luis Carlos]]></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[Thierry]]></surname>
<given-names><![CDATA[Calmus]]></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[González-León]]></surname>
<given-names><![CDATA[Carlos]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad Nacional Autónoma de México Posgrado en Ciencias de la Tierra Estación Regional del Noroeste]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad Nacional Autónoma de México Instituto de Geología ]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Universidad de Sonora Departamento de Geología ]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
<country>Mexico</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>00</month>
<year>2005</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>00</month>
<year>2005</year>
</pub-date>
<volume>22</volume>
<numero>3</numero>
<fpage>345</fpage>
<lpage>357</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1026-87742005000300345&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1026-87742005000300345&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1026-87742005000300345&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN El pórfido de molibdeno El Crestón, ubicado al suroeste del poblado de Opodepe en Sonora central, es un depósito poco común en el cinturón de pórfidos cupríferos del noroeste de México. Este depósito está mayormente hospedado por un complejo de rocas metamórficas y plutónicas del Paleopro-terozoico, caracterizadas por el Granito Crestón, el cual dio una edad U-Pb en zircones de 1,730 Ma. La mineralización está asociada con un tronco porfídico de carácter subvolcánico, el cual se emplazó hace ~53 Ma durante el enfriamiento de uno de los batolitos laramídicos más extensos del Estado de Sonora. Las reservas estimadas para este depósito son relativamente pequeñas, en el orden de los 100 millones de toneladas, pero los valores de molibdeno son altos y alcanzan hasta 0.16%. La minerali-zación está diseminada en forma de sulfuros en zonas de &#8216;stockwork&#8217;, brechas hidrotermales, así como en un horizonte de enriquecimiento secundario relativamente delgado caracterizado por calcosita. La mineralización primaria consiste en molibdenita y calcopirita asociadas a zonas de alteración fílica y potásica. La estructura actual del depósito es muy compleja, principalmente debido a los efectos de la deformación relacionada con la extensión terciaria, que segmentó y rotó el cuerpo mineralizado ori-ginal. En el área de El Crestón, esta deformación está representada por fallas orientadas en dirección NE-SW y aproximadamente N-S, las cuales son características del sistema tectónico de Cuencas y Sierras (Basin and Range).]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT El Crestón molybdenum porphyry, located southwest of the town of Opodepe in central Sonora, is an uncommon deposit within the porphyry copper belt of northwestern Mexico. This deposit is mostly hosted by a complex of Paleoproterozoic rocks characterized by the Crestón Granite, which yielded a U-Pb zircon age of 1,730 Ma. The mineralization is associated with a porphyry stock of sub-volcanic character, which was emplaced ~53 Ma ago during the cooling of one of the largest Laramide batholiths in the state of Sonora. The estimated reserves for this deposit are relatively small, in the order of 100 million tons, but molybdenum grades are high and reach up to 0.16%. The mineralization is disseminated as sulfides in stockwork zones, hydrothermal breccias, as well as in a relatively thin secondary enrichment blanket characterized by chalcosite. The primary mineralization consists of molibdenite and chalcopyrite associated with phyllic and potassic alteration zones. The actual structure of the deposit is quite complex mainly due to the effects of deformation related to the Tertiary extension, which dissected and rotated the original ore body. In the area of El Crestón, this deformation is represented by NE-SW and nearly N-S oriented faults, which are characteristic of the Basin and Range province.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[El Crestón]]></kwd>
<kwd lng="es"><![CDATA[molibdeno]]></kwd>
<kwd lng="es"><![CDATA[pórfidos cupríferos]]></kwd>
<kwd lng="es"><![CDATA[Larámide]]></kwd>
<kwd lng="es"><![CDATA[Sonora]]></kwd>
<kwd lng="es"><![CDATA[México]]></kwd>
<kwd lng="en"><![CDATA[El Crestón]]></kwd>
<kwd lng="en"><![CDATA[molibdenum]]></kwd>
<kwd lng="en"><![CDATA[copper porphyries]]></kwd>
<kwd lng="en"><![CDATA[Laramide]]></kwd>
<kwd lng="en"><![CDATA[Sonora]]></kwd>
<kwd lng="en"><![CDATA[Mexico]]></kwd>
</kwd-group>
</article-meta>
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