<?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>S1405-33222021000100018</article-id>
<article-id pub-id-type="doi">10.18268/bsgm2021v73n1a121220</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[Comment to "Porphyry-related high-sulfidation mineralization early in Central American Arc Development: Cerro Quema deposit, Azuero Peninsula, Panama" by Perelló et al., (2020)]]></article-title>
<article-title xml:lang="es"><![CDATA[Comentario a "Mineralización de alta sulfuración en relación con pórfidos en el desarrollo del Arco Centroamericano: El depósito de Cerro Quema, Península de Azuero, Panamá" por Perelló et al., (2020)]]></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-group>
<aff id="Af1">
<institution><![CDATA[,James Cook University College of Science and Engineering Economic Geology Research Centre]]></institution>
<addr-line><![CDATA[Townsville ]]></addr-line>
<country>Australia</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>00</month>
<year>2021</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>00</month>
<year>2021</year>
</pub-date>
<volume>73</volume>
<numero>1</numero>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1405-33222021000100018&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1405-33222021000100018&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1405-33222021000100018&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT The Cerro Quema Au-Cu deposit is hosted by a dacite dome complex of the Río Quema Formation, a Late Campanian-Maastrichtian volcano-sedimentary sequence of the Panamanian magmatic arc. Its formational age is constrained at ~49 Ma by field evidences, crosscutting relationships and 40Ar/39Ar geochronology (Corral et al., 2016, Corral, 2021). The recent molybdenite Re-Os dates by Perelló et al. (2020) claim that ore is spatially and temporally related to the host volcanic domes at ~71 Ma. After a thorough review of the geologic, geochemical and geochronological data from the Cerro Quema area, it is concluded that the Re-Os dates of Perelló et al. (2020) are not representative of the Cerro Quema formational age. Their proposed formational age at ~71 Ma is significantly older than the age of the host rock (~67 Ma). Furthermore, they invoke a previously unrecognized regional-scale magmatic event solely based on their molybdenite Re-Os dates. Instead, the Cerro Quema genetic model discussed here, in which magmatic-hydrothermal fluids derived from porphyry copper-like intrusions associated with the Valle Rico batholith produced the Au-Cu mineralization at ~49 Ma, is consistent with the geology, geochemistry and geochronology of the Azuero Peninsula.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN El yacimiento de Au-Cu de Cerro Quema está encajado en el complejo de domos dacíticos de la Formación Río Quema, una secuencia volcanosedimentaria de edad Campaniense-Maastrichtiense del arco magmático de Panamá. Su edad de formación de ~49 Ma ha .sido determinada mediante evidencias de campo, relaciones de corte y geocronología 40Ar/39Ar (Corral et al., 2016, Corral, 2021). Las recientes edades de Re-Os en molibdenita presentadas por Perelló et al. (2020) afirman que la mineralization está relacionada espacial y temporalmente con los domos volcánicos, que actúan como roca caja, hace ~71 Ma. Después de una revisión exhaustiva de los datos geológicos, geoquímicos y geocronológicos del área de Cerro Quema, se concluye que las edades Re-Os de Perelló et al. (2020) no son representativas de la edad de formación de Cerro Quema. La edad de formación propuesta de ~71 Ma es significativamente más antigua que la edad de la roca caja (~67 Ma). Además, se propone un evento magmático a escala regional previamente no reconocido basándose únicamente en edades Re-Os en molibdenita. En cambio, el modelo genético de Cerro Quema discutido aquí, donde los fluidos magmáticos-hidrotermales derivados de intrusiones tipo pórfido cuprífero asociadas al batolito de Valle Rico produjeron la mineralización de oro-cobre hace ~49 Ma, es consistente con la geología, geoquímica y geocronología de la Península de Azuero.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[Alunite 40Ar/39Ar dating]]></kwd>
<kwd lng="en"><![CDATA[Cerro Quema]]></kwd>
<kwd lng="en"><![CDATA[Gold-copper]]></kwd>
<kwd lng="en"><![CDATA[Porphyry-related high-sulfidation]]></kwd>
<kwd lng="en"><![CDATA[Panama]]></kwd>
<kwd lng="es"><![CDATA[Datación 40Ar/39Ar de alunita]]></kwd>
<kwd lng="es"><![CDATA[Cerro Quema]]></kwd>
<kwd lng="es"><![CDATA[Oro-cobre]]></kwd>
<kwd lng="es"><![CDATA[Alta sulfuración relacionado con pórfidos]]></kwd>
<kwd lng="es"><![CDATA[Panamá]]></kwd>
</kwd-group>
</article-meta>
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