<?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>S1993-80122023000200088</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Caracterización petrográfica de una secuencia de rocas metamorfizadas de Calentura Arriba (Moa)]]></article-title>
<article-title xml:lang="en"><![CDATA[Petrographic characterization of a metamorphosed rocks sequence from Calentura Arriba (Moa)]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Espinosa-Borges]]></surname>
<given-names><![CDATA[Angel Eduardo]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Carballo-Peña]]></surname>
<given-names><![CDATA[Alain]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Matos-Pérez]]></surname>
<given-names><![CDATA[Keilín]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<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[González-Romero]]></surname>
<given-names><![CDATA[José Antonio]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad de Las Tunas  ]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
<country>Cuba</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad de Moa  ]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
<country>Cuba</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>06</month>
<year>2023</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>06</month>
<year>2023</year>
</pub-date>
<volume>39</volume>
<numero>2</numero>
<fpage>88</fpage>
<lpage>107</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://scielo.sld.cu/scielo.php?script=sci_arttext&amp;pid=S1993-80122023000200088&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://scielo.sld.cu/scielo.php?script=sci_abstract&amp;pid=S1993-80122023000200088&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://scielo.sld.cu/scielo.php?script=sci_pdf&amp;pid=S1993-80122023000200088&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN La caracterización petrográfica de la secuencia de rocas ofiolíticas y metamorfizadas de un sector de Calentura Arriba en el municipio de Moa, constituye una contribución para la actualización del mapa geológico de la parte suroeste de la hoja cartográfica 5277-IV &#8220;Moa&#8221;. Secciones delgadas de las secuencias de rocas metamorfizadas de Calentura Arriba se analizaron bajo microscopio de luz polarizada. En la secuencia de metagabros se identificó la paragénesis mineral compuesta por enstatitas+ augita + labradorita+ olivino+ clorita+ garnierita + actinolita + tremolita + ilmenita + magnetita + sericita+ saussurita. En la secuencia de serpentinitas se identificó la paragénesis mineral compuesta por olivino+ ortopiroxenos+ bastita + lizardita + crisotilo + actinolita + tremolita + antigorita + serpofita + cromita +magnetita. Este sector estuvo sometido a fuertes procesos de transformación reflejado en las intensas alteraciones que denotan la ocurrencia de un metamorfismo de grado bajo a alto grado, coincidiendo con la serie de las facies barrowiense. Las transformaciones metamórficas están en estrecha relación con la actividad de la Falla Moa y denotan un carácter regional, extendiéndose en ambos extremos de esta fractura.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT The petrographic characterization of ophiolitic sequence and metamorphized rocks of Calentura Arriba sector in Moa municipality, constitutes a contribution to the updating of the geological map of the southwestern part of cartographic sheet 5277-IV &#8220;Moa&#8221;. Thin sections of those rocks were analyzed using a polarized light microscope. The ore paragenesis composed of enstatites + augite + labradorite + olivine + chlorite + garnierite + actinolite + tremolite + ilmenite + magnetite + sericite + saussurite in the metagabbro sequence was identified as well as the mineral paragenesis composed of olivine + orthopyroxenes + bastite + lizardite + chrysotile + actinolite + tremolite + antigorite + serpophite + chromite + magnetite in the serpentinite sequence. This sector was subjected to strong transformation processes reflected in the intense alterations that denote the occurrence of low-grade to high-grade metamorphism, matching with the Barrowian facies series. The metamorphic transformations are closely related to the activity of the Moa Fault and denote a regional character, extending at both ends of this fracture.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[petrografía]]></kwd>
<kwd lng="es"><![CDATA[rocas metamorfizadas]]></kwd>
<kwd lng="es"><![CDATA[ofiolitas]]></kwd>
<kwd lng="es"><![CDATA[Calentura Arriba]]></kwd>
<kwd lng="es"><![CDATA[Moa]]></kwd>
<kwd lng="en"><![CDATA[petrography]]></kwd>
<kwd lng="en"><![CDATA[metamorphosed rocks]]></kwd>
<kwd lng="en"><![CDATA[ophiolites]]></kwd>
<kwd lng="en"><![CDATA[Moa]]></kwd>
</kwd-group>
</article-meta>
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