<?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>1026-8774</journal-id>
<journal-title><![CDATA[Revista mexicana de ciencias geológicas]]></journal-title>
<abbrev-journal-title><![CDATA[Rev. mex. cienc. geol]]></abbrev-journal-title>
<issn>1026-8774</issn>
<publisher>
<publisher-name><![CDATA[Universidad Nacional Autónoma de México, Instituto de Geología]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S1026-87742020000300212</article-id>
<article-id pub-id-type="doi">10.22201/cgeo.20072902e.2020.3.1585</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Litofacies y mineralogía de los depósitos de sínter de la zona geotérmica de San Agustín del Maíz, Michoacán, México]]></article-title>
<article-title xml:lang="en"><![CDATA[Lithofacies and mineralogy of sinter deposits from San Agustín del Maíz geothermal zone, Michoacán, Mexico]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Olvera-García]]></surname>
<given-names><![CDATA[Emmanuel]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
<xref ref-type="aff" rid="Aaf"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Garduño-Monroy]]></surname>
<given-names><![CDATA[Víctor Hugo]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Ostrooumov]]></surname>
<given-names><![CDATA[Mikhail]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Bermejo-Santoyo]]></surname>
<given-names><![CDATA[Gerardo]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Guevara-Alday]]></surname>
<given-names><![CDATA[Jorge Alejandro]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Brogi]]></surname>
<given-names><![CDATA[Andrea]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Liotta]]></surname>
<given-names><![CDATA[Domenico]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad Michoacana de San Nicolás de Hidalgo Instituto de Investigación en Ciencias de la Tierra ]]></institution>
<addr-line><![CDATA[Morelia Michoacán]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Università degli Studi di Bari Dipartimento di Scienze della Terra e Geoambientali ]]></institution>
<addr-line><![CDATA[Bari ]]></addr-line>
<country>Italy</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,University of Quebec in Montreal Department of Earth and Atmospheric Science ]]></institution>
<addr-line><![CDATA[Montreal ]]></addr-line>
<country>Canada</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>00</month>
<year>2020</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>00</month>
<year>2020</year>
</pub-date>
<volume>37</volume>
<numero>3</numero>
<fpage>212</fpage>
<lpage>223</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1026-87742020000300212&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1026-87742020000300212&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1026-87742020000300212&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN En la zona geotérmica de San Agustín del Maíz (Michoacán) se han identificado depósitos de sínter de sílice coexistiendo con manifestaciones hidrotermales activas. Estos depósitos, considerando el modo de deposición, se separan en bandeados de fractura y estratificados. Los primeros están asociados a los conductos a través de los cuales los fluidos ascienden a la superficie, mientras que los segundos se forman a partir de los fluidos que logran llegar a la superficie. Los depósitos estratificados presentan diferentes litofacies que se pueden agrupar en un rango con dos miembros finales: por un lado, un depósito hidrotermal puro, denso, de aspecto vítreo y compacto. Por el otro lado, un depósito hidrotermal limo-arenoso, deleznable, con impresiones de plantas y algunos líticos. El depósito vítreo se considera geiserita, formado por salmueras con temperaturas superiores a los 70 °C, mientras que el depósito limo-arenoso se considera que se ha formado por salmueras con temperaturas inferiores a los 70 °C y en algunos casos, distantes de la surgente termal. Los depósitos vítreos están constituidos mineralógicamente solo por ópalo (C y CT), mientras que los depósitos limo-Fiuarenosos están formados por ópalo en conjunto con otras fases mineralógicas asociadas a sedimentos. Se ha establecido que las litofacies y la mineralogía de los depósitos de sínter de sílice pueden dar información de las temperaturas y las tasas de deposición de las surgentes hidrotermales que les dieron origen. Esta información es de utilidad para la identificación de áreas donde existió mayor emergencia de fluidos hidrotermales a la superficie y con mayor temperatura (e.g. facies de geiserita), especialmente en zonas geotérmicas con un contexto geológico similar al de San Agustín del Maíz (e.g. sector central del Cinturón Volcánico Trans-Mexicano). Dichas áreas con importante circulación de fluidos pueden coincidir localmente con intersección de fallas, terminación de fallas y rampas de relevo.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT In the active San Agustín del Maíz geothermal zone (Michoacán), we identified silica-sinter deposits co-existing with hot springs. Considering the deposition mode, these deposits are separated into fracture-banded and bedded deposits. The first ones are associated with deposition on the channels from the fluids rising to the surface, while the second ones are formed from the geothermal fluids that reached the surface. The bedded deposits showed different types of lithofacies grouped in a range with two endmembers: on the one hand, a pure silica-sinter deposit characterized by high density, glassy aspect and being consolidated. On the other hand, a silty-sandy deposit, that easily disaggregate, presenting impression of plants and lithics. The vitreous deposit is considered geyserite, formed from fluids with temperatures superior to 70 °C, while the silty-sandy deposits are formed from fluids with temperatures below 70 °C and, in some cases, far away from the water source. The geyserite deposits are mineralogically composed only by opal (C and CT), while the silty-sandy deposits are formed by opal in association with other mineralogical phases (linked to sediments). Consequently, we recognized that the lithofacies and the mineralogy of the silica-sinter deposits give information of the temperatures and deposition rates of the parental fluids. This information could be very useful in order to identify setting where existed grater geothermal up flow and temperature (e.g. geiserite facies) in areas with similar geological context to San Agustín del Maíz (e.g. central sector of the Cinturón Volcánico Trans-Mexicano). These sceneries can be associated to structural settings like fault intersections, fault-tips and relay-ramps.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[sínter de sílice]]></kwd>
<kwd lng="es"><![CDATA[ópalo]]></kwd>
<kwd lng="es"><![CDATA[litofacies]]></kwd>
<kwd lng="es"><![CDATA[mineralogía]]></kwd>
<kwd lng="en"><![CDATA[silica-sinter]]></kwd>
<kwd lng="en"><![CDATA[opal]]></kwd>
<kwd lng="en"><![CDATA[lithofacies]]></kwd>
<kwd lng="en"><![CDATA[mineralogy]]></kwd>
</kwd-group>
</article-meta>
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