<?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>S1405-33222018000200549</article-id>
<article-id pub-id-type="doi">10.18268/bsgm2018v70n2a14</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[Trace-metal content of the Cerro Quema Au-Cu deposit (Azuero Peninsula, Panama): Implications for exploration]]></article-title>
<article-title xml:lang="es"><![CDATA[Contenido en metales trazas del depósito Au-Cu de Cerro Quema (península de Azuero, Panamá): Implicaciones para la exploración]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Corral]]></surname>
<given-names><![CDATA[Isaac]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Corbella]]></surname>
<given-names><![CDATA[Mercè]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Gómez-Gras]]></surname>
<given-names><![CDATA[David]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Griera]]></surname>
<given-names><![CDATA[Albert]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,James Cook University College of Science and Engineering Economic Geology Research Centre]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
<country>Australia</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universitat Autònoma de Barcelona Departament de Geologia ]]></institution>
<addr-line><![CDATA[Barcelona ]]></addr-line>
<country>Spain</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>00</month>
<year>2018</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>00</month>
<year>2018</year>
</pub-date>
<volume>70</volume>
<numero>2</numero>
<fpage>549</fpage>
<lpage>565</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1405-33222018000200549&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1405-33222018000200549&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1405-33222018000200549&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract Cerro Quema (Azuero Peninsula, Panama) is a high-sulfidation epithermal Au-Cu deposit hosted by a dacite dome complex of the Río Quema Formation (late Campanian to Maastrichtian). High-sulfidation mineralization at Cerro Quema occurs within a lithocap of vuggy quartz and advanced argillic alteration, and comprises a first stage of disseminations and microveinlets of pyrite, chalcopyrite, enargite, tennantite, and minor sphalerite. This stage is crosscut by younger veins that contain quartz, barite, pyrite, chalcopyrite, sphalerite, and galena. Later weathering and oxidation processes have produced two distinct mineralized zones at Cerro Quema: (1) Sulfide ore zone-a deeper zone of hypogene alteration and sulfide mineralization with some secondary enrichment but unaffected by oxidation, and (2) Oxide ore zone-a thick iron oxide-rich zone that overprints the hypogene alteration/ mineralization in the upper ~150 m of the deposit. To characterize the concentrations and distribution of metals in the two ore zones, and to develop geochemical tools for exploration, we analyzed 34 samples of both oxide (n = 23) and sulfide ore (n = 11) for Au, Ag, Cd, Cu, Mn, Mo, Ni, Pb, Zn, S, As, Ba, Hg, Sb, and W by INAA and ICP-MS. The results show that the oxide ore has the highest concentration of Au (2.4 g/t), Ag (2.0 g/t), Pb (432 ppm), and Sb (317 ppm), whereas the sulfide ore has the highest concentration of Cu (&gt; 1%), Zn (403 ppm), As (2.74%), and Cd (15.2 ppm). The enrichment factor calculation (oxide/ sulfide ore) indicate that Au, Ag, Pb, and Sb are concentrated in the oxide zone whereas Cu, Zn, Ba, Ni, As, and S are concentrated in the sulfide zone. Exploration for Au should target the oxide ore zone, in areas where the Ba concentration is also high. Exploration for Cu should target the sulfide ore zone, below the oxidation boundary, where primary and secondary Cu sulfides coexist.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen Cerro Quema (Península de Azuero, Panamá) es un depósito epitermal de alta sulfuración de Au-Cu hospedado en el complejo de domos dacíticos de la Formación Río Quema (Campaniense Superior - Maastrichtiense). La mineralización de tipo epitermal de alta sulfuración en Cerro Quema ocurre en un lithocap de cuarzo vuggy y alteración argílica avanzada, y está compuesta por un primer estadio de diseminaciones y microvetas de pirita, calcopirita, enargita, tennantita y en menor cantidad esfalerita. Este tipo de mineralización está cortada por un segundo estadio más joven de vetillas que contienen cuarzo, barita, pirita, calcopirita, esfalerita y galena. Posteriormente, los procesos de meteorización y oxidación produjeron dos zonas mineralizadas distintas en Cerro Quema; (1) Zona de sulfuros: zona más profunda del yacimiento, caracterizada por alteración/mineralización hipogénica, con menor grado de enriquecimiento secundario pero libre de óxidos, y (2) Zona de óxidos: zona superficial caracterizada por óxidos de hierro, desarrollada hasta ~150 m de profundidad y sobreimpuesta a la alteración/mineralización hipogénica. Para caracterizar la concentración y distribución de metales en las dos zonas mineralizadas, como también para desarrollar herramientas de exploración geoquímica, hemos analizado la concentración de Au, Ag, Cd, Cu, Mn, Mo, Ni, Pb, Zn, S, As, Ba, Hg, Sb, y W mediante INAA e ICP-MS en 34 muestras de ambas zonas mineralizadas, óxidos (n = 23) y sulfuros (n = 11). Los resultados muestran que la zona de óxidos tiene la concentración más elevada de Au (2.4 g/t), Ag (2.0 g/t), Pb (432 ppm), y Sb (317 ppm), mientras que la zona de sulfuros tiene la concentración más elevada de Cu (&gt; 1%), Zn (403 ppm), As (2.74%), y Cd (15.2 ppm). El cálculo del factor de enriquecimiento (óxidos/sulfuros) indica que el Au, Ag, Pb y Sb se concentran en la zona de óxidos, mientras el Cu, Zn, Ba, Ni, As y S se concentran en la zona de sulfuros. La exploración de Au en este tipo de depósitos debe centrarse en la zona de óxidos, donde la concentración de Ba es también elevada. Por el contrario, la exploración de Cu en este tipo de depósitos debe centrarse en la zona de sulfuros, por debajo de la zona de oxidación, donde coexisten tanto sulfuros primarios como sulfuros secundarios.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[Exploration]]></kwd>
<kwd lng="en"><![CDATA[Epithermal]]></kwd>
<kwd lng="en"><![CDATA[Cerro Quema]]></kwd>
<kwd lng="en"><![CDATA[Gold-Copper]]></kwd>
<kwd lng="en"><![CDATA[Panama]]></kwd>
<kwd lng="es"><![CDATA[Exploración]]></kwd>
<kwd lng="es"><![CDATA[Epitermal]]></kwd>
<kwd lng="es"><![CDATA[Cerro Quema]]></kwd>
<kwd lng="es"><![CDATA[Oro-Cobre]]></kwd>
<kwd lng="es"><![CDATA[Panamá]]></kwd>
</kwd-group>
</article-meta>
</front><back>
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