<?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>S1405-33222016000200365</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[Geochronology of Mexican mineral deposits. V: the Peñón Blanco epithermal deposit Durango]]></article-title>
<article-title xml:lang="es"><![CDATA[Geocronología de depósitos minerales mexicanos. V: Los depósitos epitermales de Peñón Blanco, Durango]]></article-title>
</title-group>
<contrib-group>
<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[Albinson]]></surname>
<given-names><![CDATA[Tawn]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Iriondo]]></surname>
<given-names><![CDATA[Alexander]]></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 ]]></institution>
<addr-line><![CDATA[CDMX ]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Exploraciones del Altiplano, S.A. de C.V.  ]]></institution>
<addr-line><![CDATA[CDMX ]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Universidad Nacional Autónoma de México Centro de Geociencias ]]></institution>
<addr-line><![CDATA[Querétaro Qro.]]></addr-line>
<country>Mexico</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>08</month>
<year>2016</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>08</month>
<year>2016</year>
</pub-date>
<volume>68</volume>
<numero>2</numero>
<fpage>365</fpage>
<lpage>370</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1405-33222016000200365&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1405-33222016000200365&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1405-33222016000200365&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract The low sulfidation epithermal deposits of the San Juan de Mogotes mineralized area in the Peñón Blanco district, central-eastern Durango, were dated in this study at 31.29 ± 0.08 Ma (adularia from crustiform veins, 40Ar/39Ar plateau age). Therefore, these deposits belong to the most productive metallogenic epoch-Oligocene-and are found in the most heavily mineralized region of Mexico-the western half of the Mesa Central, particularly around the San Luis-;Tepehuanes fault zone and near its confluence with the Transversal de Parras (or Parras Transversal zone). At that time and in this region epithermal deposits and tin veins in association with fluorine-rich rhyolites (highly differentiated rhyolites) were the dominant types of deposits, and both occurred at a district scale, which is the case of the Peñón Blanco district, among others. Such characteristics suggest a possible genetic link between both types of deposits, research that would need to be specifically addressed in the future.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen Los depósitos epitermales de baja sulfuración del área mineralizada de San Juan de Mogotes en el distrito de Peñón Blanco, Durango centro-oriental, son fechados en este estudio en 31.29 ± 0.08 Ma (adularia de vetas crustiformes, edad de meseta 40Ar/39Ar). Por lo tanto, estos depósitos pertenecen a la época metalogenética más productiva-oligocénica-y se encuentran en el área más densamente mineralizada de México-la mitad occidental de la Mesa Central, particularmente alrededor de la zona de falla de San Luis-;Tepehuanes y cerca de la confluencia entre ésta y la Transversal de Parras. Durante dicha época y en esta región, las tipologías dominantes de yacimientos minerales son los depósitos epitermales y las vetas de estaúo en asociación con riolitas ricas en flúor (riolitas altamente diferenciadas), y ambas tipologías se encuentran también a escala de distrito, que es el caso del distrito de Peñón Blanco, entre otros. Tales características sugieren un posible nexo genético entre ambas tipologías, tema que necesitaría ser investigado específicamente en el futuro.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[Peñón Blanco]]></kwd>
<kwd lng="en"><![CDATA[Durango]]></kwd>
<kwd lng="en"><![CDATA[Mexico]]></kwd>
<kwd lng="en"><![CDATA[epithermal deposits]]></kwd>
<kwd lng="en"><![CDATA[low sulfidation]]></kwd>
<kwd lng="en"><![CDATA[40Ar/39Ar ages]]></kwd>
<kwd lng="en"><![CDATA[adularia]]></kwd>
<kwd lng="es"><![CDATA[Peñón Blanco]]></kwd>
<kwd lng="es"><![CDATA[Durango]]></kwd>
<kwd lng="es"><![CDATA[México]]></kwd>
<kwd lng="es"><![CDATA[depósitos epitermales]]></kwd>
<kwd lng="es"><![CDATA[sulfuración baja]]></kwd>
<kwd lng="es"><![CDATA[edades 40Ar/39Ar]]></kwd>
<kwd lng="es"><![CDATA[adularia]]></kwd>
</kwd-group>
</article-meta>
</front><back>
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