<?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>1794-6190</journal-id>
<journal-title><![CDATA[Earth Sciences Research Journal]]></journal-title>
<abbrev-journal-title><![CDATA[Earth Sci. Res. J.]]></abbrev-journal-title>
<issn>1794-6190</issn>
<publisher>
<publisher-name><![CDATA[Universidad Nacional de Colombia]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S1794-61902018000300151</article-id>
<article-id pub-id-type="doi">10.15446/esrj.v22n3.63442</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[Microthermometry and Raman spectroscopy of fluid inclusions from El Vapor gold mineralizations, Colombia]]></article-title>
<article-title xml:lang="es"><![CDATA[Microtermometría y espectroscopia Raman de inclusiones fluidas de las mineralizaciones auríferas de El Vapor, Colombia]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Dorado]]></surname>
<given-names><![CDATA[Camilo E.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Molano]]></surname>
<given-names><![CDATA[Juan C.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad Nacional de Colombia  ]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
<country>Colombia</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>09</month>
<year>2018</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>09</month>
<year>2018</year>
</pub-date>
<volume>22</volume>
<numero>3</numero>
<fpage>151</fpage>
<lpage>158</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.co/scielo.php?script=sci_arttext&amp;pid=S1794-61902018000300151&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.co/scielo.php?script=sci_abstract&amp;pid=S1794-61902018000300151&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.co/scielo.php?script=sci_pdf&amp;pid=S1794-61902018000300151&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT Epigenetic El Vapor gold mineralization is hosted by the Segovia batholith and sedimentary rocks at both sides of El Nús fault, in the eastern flank of the Colombian Andes central cordillera. Gold mineralization is composed by continuous and discontinuous sigmoidal and stockwork veins and veinlets from a few centimeters to two meters of thickness and by hydrothermal breccias. Ore mineralogy includes Pyrite + Galena + Sphalerite ± Chalcopyrite ± Pyrrhotite + Proustite - Pyrargyrite. Gold occurs as inclusions within pyrite, between quartz crystals and filling fractures within pyrite at a late stage of mineralization. The fluid inclusions in quartz veins occur as clusters of primary inclusions or in alignments of secondary and pseudo-secondary inclusions. Based on petrography and Raman spectroscopy, four types of fluid inclusions could be recognized: (1) Type I are primary biphasic, liquid-rich, with (2) Type II are primary or pseudosecondary, multi-volatile presenting (3) Type III are secondary, two-phase, liquid-rich inclusions, composed of  and have two different times of formation (IIIA and IIIB), (4) Type IV are very rare, three-phasic, secondary inclusions and composed of S   The microthermometric and spectroscopic analysis of fluid inclusions indicates that the fluid associated with the first event of mineralization identified in El Vapor have low to moderate salinities (3.5-9.2 wt% NaCl equiv.), with trapping temperatures between 214°C and 350°C and pressures between 0.5kbar and 2.9kbar. Due to the nonexistence of fluid inclusions with variable degree of filling with opposite homogenization and because of the variations of salinity in a restricted homogenization temperatures range, it is proposed an isothermal fluid mixture process, which together with fO2 changes, generated by fluid reaction with the carbonaceous shales of the Segovia sedimentary rocks, could influence the process of gold deposition. Hydrothermal fluids from El Vapor were near neutral and reduced; similar features have been found in orogenic deposits hosted by turbidite sequences around the world.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN Las mineralizaciones epigenéticas de El Vapor se encuentran hospedadas en el Batolito de Segovia y rocas sedimentarias a ambos lados de la falla de El Nús, en el flanco oriental de la Cordillera Central de los Andes Colombianos. Las mineralizaciones auríferas están compuestas por venas y vetillas continuas y discontinuas, sigmoidales y en stockwork desde pocos centímetros hasta dos metros de espesor, así como por brechas hidrotermales. Los minerales de mena incluyen Pirita + Galena + Esfalerita ± Calcopirita ± Pirrotina + Proustita - Pirargirita. Oro se presenta como inclusiones dentro de pirita, entre cristales de cuarzo y rellenando fracturas dentro de pirita, en un estadio tardío de mineralización. Las inclusiones fluidas en las venas de cuarzo se presentan como agrupaciones de inclusiones primarias como alineaciones de inclusiones secundarias y pseudo-secundarias. Con base en petrografía y espectroscopia Raman, se identificaron cuatro tipos de inclusiones: (1) Tipo I, primarias, bifásicas, ricas en líquido, con  (2) Tipo II, primarias o pseudo-secundarias, multivolátiles, con presencia de  (3) Tipo III, secundarias, bifásicas, ricas en líquido, compuestas por  con dos temporalidades diferentes (IIIA y IIIB), (4) Tipo IV, muy escasas, de tres fases, secundarias y compuestas por . Los análisis microtermométricos y espectroscópicos de las inclusiones fluidas indican que el fluido hidrotermal relacionado con el primer evento de mineralización identificado en el El Vapor, presenta una salinidad baja a moderada (3.5-9.2 wt% NaCl equiv.), temperaturas de entrampamiento entre 214°C y 350°C y presiones mínimas de entrampamiento entre 0.5kbar y 2.9kbar. Debido a la inexistencia de inclusiones fluidas con grados variables de relleno y modos diferentes de homogenización, y teniendo en cuenta las variaciones de salinidad observadas en un rango restringido de temperaturas de homogenización, se propone que un proceso de mezcla isotermal de fluidos, junto con cambios en la fugacidad de oxígeno, generadas por la reacción de los fluidos con los shales carbonosos de las rocas sedimentarias de Segovia, pudieron influenciar el proceso de depósito del oro. Los fluidos hidrotermales en El Vapor fueron reducidos y cercanos a la neutralidad, características similares han sido encontradas en depósitos orogénicos hospedados en secuencias turbidíticas alrededor del mundo.]]></p></abstract>
<kwd-group>
<kwd lng="en"><![CDATA[Fluid inclusions]]></kwd>
<kwd lng="en"><![CDATA[Microthermometry]]></kwd>
<kwd lng="en"><![CDATA[Raman spectroscopy]]></kwd>
<kwd lng="en"><![CDATA[Gold mineralizations]]></kwd>
<kwd lng="en"><![CDATA[El Vapor district]]></kwd>
<kwd lng="en"><![CDATA[reduced fluids]]></kwd>
<kwd lng="en"><![CDATA[Orogenic]]></kwd>
<kwd lng="es"><![CDATA[Inclusiones fluidas]]></kwd>
<kwd lng="es"><![CDATA[Microtermometría]]></kwd>
<kwd lng="es"><![CDATA[Espectroscopia Raman]]></kwd>
<kwd lng="es"><![CDATA[Mineralizaciones Auríferas]]></kwd>
<kwd lng="es"><![CDATA[Distrito de El Vapor]]></kwd>
<kwd lng="es"><![CDATA[Fluidos Reducidos]]></kwd>
<kwd lng="es"><![CDATA[Orogénico]]></kwd>
</kwd-group>
</article-meta>
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