<?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>S1405-33222021000100019</article-id>
<article-id pub-id-type="doi">10.18268/bsgm2021v73n1a101220</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[Reply to "Porphyry-related high-sulfidation mineralization early in Central American Arc development: Cerro Quema deposit, Azuero Peninsula, Panama" by Corral (2021)]]></article-title>
<article-title xml:lang="es"><![CDATA[Respuesta 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 Corral (2021)]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Perelló]]></surname>
<given-names><![CDATA[José]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Creaser]]></surname>
<given-names><![CDATA[Robert A.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[García]]></surname>
<given-names><![CDATA[Alfredo]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Antofagasta Minerals S.A.  ]]></institution>
<addr-line><![CDATA[Santiago ]]></addr-line>
<country>Chile</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,University of Alberta Department of Earth and Atmospheric Sciences ]]></institution>
<addr-line><![CDATA[Edmonton Alberta]]></addr-line>
<country>Canada</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Santiago  ]]></institution>
<addr-line><![CDATA[Santiago ]]></addr-line>
<country>Chile</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=S1405-33222021000100019&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1405-33222021000100019&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1405-33222021000100019&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT Dear Editor, we thank Corral (2020) for his anticipated interest in our paper on the timing of the porphyry-related high-sulfidation epithermal mineralization at Cerro Quema in the Azuero peninsula of southwestern Panama. Our study, based on three Re-Os ages for molybdenite intimately associated with Cu-bearing sulfide minerals from the hypogene roots of the La Pava center (Figure 1), shows that the main event of high-sulfidation Cu mineralization took place during the earliest Maastrichtian at ~71 Ma. The reported ages, together with the geologic relationships described in our paper (Perelló et al., 2020), plus a series of regional geologic, structural, petrochemical, and geotectonic considerations, not only precisely date the porphyry-related nature of the Cerro Quema high-sulfidation mineralization, but are also significant in that they confirm the rapid evolution of the earliest stages of the Central American Arc - from subduction initiation at 75-73 Ma to arc stability and maturation at 71 Ma (e.g., Buchs et al., 2011a and references therein) - and place the mineralization in a regional geodynamic setting. Irrespective of the regional geologic arguments reiterated by Corral (2020) in support of his previous genetic interpretation (e.g.,Corral et al., 2016) and to invalidate our conclusions, Corral's real concern is the reliability of our molybdenite ages, which are much older than his preferred age of mineralization for Cerro Quema. We believe that many of the points raised by Corral (2020), including the regional and local geologic backgrounds of the deposit and the dated samples, were properly addressed in Perelló et al. (2020), and that it would be redundant to repeat them here. Additional petrochemical evidence in support can be found in Whattam and Stern (2015, 2020) and Whatam (2018).]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN Estimado Editor, agradecemos a Corral (2020) por su interés anticipado en nuestro artículo sobre el momento de la mineralización epitermal de alta sulfuración en relación con el pórfido en el Cerro Quema en la península de Azuero, al suroeste de Panamá. Nuestro estudio, basado en tres edades Re-Os para la molibdenita, íntimamente asociadas con minerales de sulfuro que contienen Cu de las raíces hipógenas del centro de La Pava (Figura 1), muestra que el evento principal de la mineralización de alta sulfuración de Cu tuvo lugar durante la primera Maastrichtiense en ~71 Ma. Las edades reportadas, junto con la relación geológica descrita en nuestro artículo, (Perelló et al., 2020), además de una serie de consideraciones geológicas, estructurales, petroquímicas y geotectónicas regionales, no solo datan con precisión la naturaleza de la alta sulfuración en relación con el pórfido del Cerro Quema, sino que, además, son significativas porque confirman la rápida evolución de las primeras etapas del Arco Centroamericano- desde la iniciación de la subducción a 75-73 Ma hasta la estabilidad del arco y la maduración a 71 Ma (por ejempdo, Buchs et al., 2011a y referencias en él) - y situar la mineralización en un entorno geodinámico regional. Independientemente de los argumentos geológicos regionales reiterados por Corral (2020) en apoyo a su interpretación genética previa (por ejemplo, Corral et al., 2016)y para invalidar nuestras conclusiones, la verdadera preocupación de Corral es la cortfiabilidad de nuestras edades de molibdenita, las cuales son mucho más antiguas que su edad preferida de mineralización para el Cerro Quema. Creemos que muchos de los puntos planteados por Corral (2020), incluidos los antecedentes geológicos locales y regionales del depósitoy las muestrasfechadas, se abordaron adecuadamente en Perelló et al. (2020), por lo que repetirlos aquí sería redundante. Pueden encontrarse pruebas petroquímicas adicionales en Whattamy Stern (2015, 2020) y Whatam (2018).]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[Azuero]]></kwd>
<kwd lng="en"><![CDATA[Caribean Large Igneous Province]]></kwd>
<kwd lng="en"><![CDATA[Central American Arc]]></kwd>
<kwd lng="en"><![CDATA[High-sulfidation]]></kwd>
<kwd lng="en"><![CDATA[Molybdenite]]></kwd>
<kwd lng="es"><![CDATA[Azuero]]></kwd>
<kwd lng="es"><![CDATA[Provincia Magmática Caribeña]]></kwd>
<kwd lng="es"><![CDATA[Arco Centroamericano]]></kwd>
<kwd lng="es"><![CDATA[Alta Sulfuración]]></kwd>
<kwd lng="es"><![CDATA[Molibdenita]]></kwd>
</kwd-group>
</article-meta>
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