<?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>S1405-33222019000100207</article-id>
<article-id pub-id-type="doi">10.18268/bsgm2019v71n1a11</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[Geochronology of Mexican mineral deposits. VIII: the Zacatepec polymetallic skarn, Oaxaca]]></article-title>
<article-title xml:lang="es"><![CDATA[Geocronología de depósitos minerales mexicanos. VIII: el skarn polimetálico de Zacatepec, Oaxaca]]></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[Cabrera-Roa]]></surname>
<given-names><![CDATA[Miguel Ángel]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[González-Partida]]></surname>
<given-names><![CDATA[Eduardo]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[López-Martínez]]></surname>
<given-names><![CDATA[Margarita]]></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[,Universidad Nacional Autónoma de México  ]]></institution>
<addr-line><![CDATA[CDMX ]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Universidad Nacional Autónoma de México  ]]></institution>
<addr-line><![CDATA[Querétaro ]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af4">
<institution><![CDATA[,Centro de Investigación Científica y Educación Superior de Ensenada  ]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
<country>Mexico</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>00</month>
<year>2019</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>00</month>
<year>2019</year>
</pub-date>
<volume>71</volume>
<numero>1</numero>
<fpage>207</fpage>
<lpage>218</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1405-33222019000100207&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1405-33222019000100207&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1405-33222019000100207&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract The Zn-Pb-Ag(-W) skarn deposits at Zacatepec (or M&#616;&#616;yg&#616;xy) in Oaxaca are associated with rocks of the Sierra Madre del Sur (SMS) magmatic province, and located in its easternmost part, in southern Mexico. This region consists of Eocene to Miocene calc-alkaline hypabyssal and volcanic rocks, with intermediate to felsic compositions that intrude or overlie Cretaceous carbonate sequences. Prograde mineralization in the Zacatepec skarn deposits was dated by means of the40Ar/39Ar method in a sample of the granitic hypabyssal body, with which the formation of these deposits is directly associated. The isochron ages thus yielded are 17.52 ± 0.14 Ma for biotite and 17.33 ± 0.40 Ma for hornblende. Such ages are in accordance with several other magmatic-hydrothermal deposits (epithermal, skarn, and porphyry-type deposits) that are hosted by Miocene rocks in central Oaxaca state. Deposits in the region with known ages for Miocene hypabyssal rocks with which they are closely related are Taviche, Lachigalla, Cobre Grande, Aurena, Natividad, Altagracia-Águila-Arista, Santa Margarita-Azucena, and Guielavazar. The plausible ages for these ore deposits determine a time bracket between &lt;23.8 and &lt;13.01 Ma (early to middle Miocene) that can be considered as favorable for the finding of magmatic-hydrothermal ore deposits. The latter can be tentatively used to define a new metallogenic period that corresponds to a new metallogenic province, for which the rocks derived from the Miocene magmatism of the SMS constitute the metallotect. Although such metallogenic activity has not been altogether overlooked, no previous papers have focused on its relevance and extent in space and time. Therefore, this province constitutes the fifth Miocene mineralized region known in Mexico, besides the southernmost Sierra Madre Occidental, the Trans-Mexican Volcanic Belt, the Gulf of California, and the alkaline province in Chiapas.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen La formación de los depósitos de skarn de Zn-Pb-Ag(-W) en Zacatepec (o M&#616;&#616;yg&#616;xy) en Oaxaca está asociada a rocas de la provincia ígnea de la Sierra Madre del Sur (SMS) y estos depósitos se encuentran en su terminación más oriental, en el sur de México. Esta región está constituida esencialmente por rocas hipabisales y volcánicas calcialcalinas, con composiciones intermedias a félsicas y edades entre el Eoceno y el Mioceno que intruyen o cubren secuencias carbonatadas del Cretácico. La mineralización prógrada de los depósitos de skarn de Zacatepec fue fechada por medio del método de40Ar/39Ar en una muestra del cuerpo granítico hipabisal con el cual, la formación de estos depósitos está directamente asociada. Las edades de isócrona obtenidas son 17.52 ± 0.14 Ma para biotita y 17.33 ± 0.40 Ma para hornblenda. Dichas edades son similares a las de diversos depósitos magmático-hidrotermales (epitermales, skarns, y depósitos en pórfidos) encajonados en rocas del Mioceno en la parte central del estado de Oaxaca. Los depósitos en la región, con edades conocidas para rocas hipabisales del Mioceno con las que éstos se encuentran estrechamente relacionados son Taviche, Lachigalla, Cobre Grande, Aurena, Natividad, Altagracia-Águila-Arista, Santa Margarita-Azucena y Guielavazar. Las edades plausibles para estos depósitos minerales determinan un intervalo de tiempo entre &lt;23.8 y &lt;13.01 Ma (Mioceno temprano a medio), que puede ser considerado como favorable para el hallazgo de yacimientos minerales magmático-hidrotermales. Ello puede ser tentativamente usado para la definición de un nuevo periodo metalogenético, que corresponde a una nueva provincia metalogenética para la cual, las rocas derivadas del magmatismo miocénico de la SMS constituyen el metalotecto. Aunque dicha actividad metalogenética no ha pasado completamente desapercibida, no existen publicaciones previas enfocadas en su importancia y extensión espacial y temporal. De este modo, dicha provincia constituye la quinta región mineralizada circunscrita al Mioceno conocida en México, junto con el extremo sur de la Sierra Madre Oriental, la Faja Volcánica Mexicana, el Golfo de California y la provincia alcalina de Chiapas.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[Oaxaca]]></kwd>
<kwd lng="en"><![CDATA[Mexico]]></kwd>
<kwd lng="en"><![CDATA[skarn]]></kwd>
<kwd lng="en"><![CDATA[40Ar/39Ar ages]]></kwd>
<kwd lng="en"><![CDATA[prograde associations]]></kwd>
<kwd lng="en"><![CDATA[early Miocene]]></kwd>
<kwd lng="en"><![CDATA[Sierra Madre del Sur]]></kwd>
<kwd lng="es"><![CDATA[Oaxaca]]></kwd>
<kwd lng="es"><![CDATA[México]]></kwd>
<kwd lng="es"><![CDATA[skarn]]></kwd>
<kwd lng="es"><![CDATA[edades 40Ar/39Ar]]></kwd>
<kwd lng="es"><![CDATA[asociaciones prógradas]]></kwd>
<kwd lng="es"><![CDATA[Mioceno temprano]]></kwd>
<kwd lng="es"><![CDATA[Sierra Madre del Sur]]></kwd>
</kwd-group>
</article-meta>
</front><back>
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