<?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>1993-8012</journal-id>
<journal-title><![CDATA[Minería y Geología]]></journal-title>
<abbrev-journal-title><![CDATA[Min. Geol.]]></abbrev-journal-title>
<issn>1993-8012</issn>
<publisher>
<publisher-name><![CDATA[EDUM. Universidad de Moa]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S1993-80122019000400384</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Caracterización petrológica-geoquímica de la asociación ultramáfica del complejo ofiolítico Moa-Baracoa en el sector Camarioca Sur]]></article-title>
<article-title xml:lang="en"><![CDATA[Petrologic-geochemical characterization of ultramafic association in Camarioca Sur area of Moa-Baracoa ophiolite complex]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Valdés-Mariño]]></surname>
<given-names><![CDATA[Yurisley]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Muñoz-Gómez]]></surname>
<given-names><![CDATA[José Nicolás]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Orozco-Melgar]]></surname>
<given-names><![CDATA[Gerardo Antonio]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Blanco-Quintero]]></surname>
<given-names><![CDATA[Idael Francisco]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Pérez-García]]></surname>
<given-names><![CDATA[Luis Alberto]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Urra-Abraira]]></surname>
<given-names><![CDATA[Jorge]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad de Moa  ]]></institution>
<addr-line><![CDATA[ Holguín]]></addr-line>
<country>Cuba</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad de Alicante  ]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
<country>Spain</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Empresa Moa Nickel S.A. Pedro Sotto Alba  ]]></institution>
<addr-line><![CDATA[Moa Holguín]]></addr-line>
<country>Cuba</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>12</month>
<year>2019</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>12</month>
<year>2019</year>
</pub-date>
<volume>35</volume>
<numero>4</numero>
<fpage>384</fpage>
<lpage>399</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://scielo.sld.cu/scielo.php?script=sci_arttext&amp;pid=S1993-80122019000400384&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://scielo.sld.cu/scielo.php?script=sci_abstract&amp;pid=S1993-80122019000400384&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://scielo.sld.cu/scielo.php?script=sci_pdf&amp;pid=S1993-80122019000400384&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN Camarioca Sur es un sector de la asociación ofiolítica Moa-Baracoa compuesto por ultramafitas piroxénicas, espinelas cromíferas, anfibolitas gnéisicas y granofels anfibolíticos, en el cual se ha documentado la presencia de diques de rocas compactas y duras, de color blanco a gris oscuro, con escaso desarrollo de corteza de meteorización. Para caracterizar, petrológica y geoquímicamente, la asociación litológica ultramáfica y los diques leucocráticos asociados se analizaron secciones delgadas de doce muestras. Se encontró que las rocas ultramáficas que predominan son dunitas y harzburgitas, las que se encuentran cortadas por diques leucocráticos. Las peridotitas están compuestas por olivino principalmente, con presencia de cromo-espinelas y en menor medida piroxenos. Las rocas están parcial o totalmente transformadas a minerales del grupo de la serpentina (antigorita, lizardita y venillas de crisotilo). Algunas peridotitas están metamorfizadas, desarrollando talco + tremolita + clorita. Las rocas leucocráticas, que cortan a través de diques a las peridotitas, están constituidas principalmente por plagioclasa (oligoclasa-andesina), cuarzo y actinolita, y como accesorios aparecen moscovita, apatito y rutilo. Estos diques muestran un ligero metamorfismo, desarrollando una foliación y la formación de albita + clinozoicita + caolinita, lo que denota condiciones de un metamorfismo de grado desde bajo hasta medio.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract Camarioca Sur is a sector in Moa-Baracoa ophiolitic complex composed of pyroxene ultramaphites, gneissic amphiboles, chromium-spinels and amphibolitic granofels, in which the presence of compact and hard rock dykes has been documented, white to dark gray color and poor weathering crust development. The aim of this research is to characterize the associated leucocratic dykes and the ultramafic lithological association of Moa-Baracoa ophiolitic complex in Camarioca Sur sector by using petrological and geochemical techniques. It was found harzburgite dunites are the predominant rocks. Peridotites are mainly composed of olivine, with the presence of chromium-spinels and to lesser extent pyroxenes. The rocks are partial or totally transformed into minerals of serpentine group (antigorite, lizardite and chrysotile). Some peridotites are metamorphosed, developing talcum + tremolite + chlorite. The leucocratic rocks, which cut through the peridotite dikes, consist mainly of plagioclase (oligoclase-andesine), quartz and actinolite, and apatite, Muscovite and rutile as accessories. These dikes show a slight metamorphism, developing a foliation and the formation of albite + clinozoisite + kaolinite, which denotes conditions of metamorphism of degree from low to medium.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[asociación ofiolítica Moa-Baracoa]]></kwd>
<kwd lng="es"><![CDATA[Camarioca Sur]]></kwd>
<kwd lng="es"><![CDATA[antigorita]]></kwd>
<kwd lng="es"><![CDATA[harzburgitas]]></kwd>
<kwd lng="es"><![CDATA[dunitas]]></kwd>
<kwd lng="es"><![CDATA[rocas leucocráticas]]></kwd>
<kwd lng="en"><![CDATA[Moa-Baracoa ophiolitic association]]></kwd>
<kwd lng="en"><![CDATA[Camarioca Sur]]></kwd>
<kwd lng="en"><![CDATA[antigorite]]></kwd>
<kwd lng="en"><![CDATA[harzburgite]]></kwd>
<kwd lng="en"><![CDATA[dunites]]></kwd>
<kwd lng="en"><![CDATA[leucocratic rocks]]></kwd>
</kwd-group>
</article-meta>
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