<?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>S1026-87742022000100001</article-id>
<article-id pub-id-type="doi">10.22201/cgeo.20072902e.2022.1.1632</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Implicaciones tectono-metamórficas bajo una dinámica de compresión en Faja Cangre, occidente de Cuba]]></article-title>
<article-title xml:lang="en"><![CDATA[Metamorphic-tectonic implications under a compression dynamic in Cangre Belt, western of Cuba]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Cáceres Govea]]></surname>
<given-names><![CDATA[Dámaso]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Cruz-Gámez]]></surname>
<given-names><![CDATA[Esther M.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad de Pinar del Río Departamento de Geología ]]></institution>
<addr-line><![CDATA[Pinar del Río ]]></addr-line>
<country>Cuba</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>00</month>
<year>2022</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>00</month>
<year>2022</year>
</pub-date>
<volume>39</volume>
<numero>1</numero>
<fpage>1</fpage>
<lpage>15</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1026-87742022000100001&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1026-87742022000100001&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1026-87742022000100001&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN La Faja Cangre se localiza en el occidente de Cuba y es parte del basamento Mesozoico de la Isla. Está constituida por tres unidades tectónicas: Pino Solo, Mestanza y Cerro de Cabras, las que descansan mediante un plano de cabalgamiento sobre la Unidad Alturas de Pizarra del Sur en el terreno Guaniguanico. Su complejo cuadro tectono-metamórfico contrasta con el resto del terreno. Las conclusiones que se presentan en este trabajo sobre la Faja Cangre están sustentadas por datos cartográficos, estructurales y petrográficos colectados por los autores durante décadas de trabajo en el área, además incluye contenidos de química mineral en micas de los siliciclastos. La rotación horaria del máximo esfuerzo compresivo &#963;  1 evoluciona con consecuencias espacio-temporales singulares, que permiten separar los aquí definidos períodos deformacionales (P), desde NW 330°-340° hasta NE 20°-30°, durante la compresión (P1) y el desarrollo del transporte tectónico (P2 y P4). La falla Pinar, reconocida como transcurrente siniestra (P3), determina el surgimiento y estilo tectónico de la faja, a partir de un ligero cambio de rumbo en el trazado de la misma, que provocó la transpresión en determinado sector, la aparición de una estructura en flor positiva (orógeno extrusivo) y su configuración definitiva durante el último período deformacional (P4). En estas condiciones tectónicas se dan varios procesos metamórficos: mc-metamorfismo vinculado al clivaje de muy bajo grado, desarrollado en todos los períodos; mt-metamorfismo por transpresión, progresivo de grado bajo y presión media- parte alta (P4, se alcanzan los mayores gradientes de P/T) y me-metamorfismo por extrusión tectónica, retrogrado de grado bajo y presión media- parte intermedia (P4). La heterogeneidad metamórfica es determinada por el emplazamiento yuxtapuesto de las secuencias extruidas.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT The Cangre Belt is located in western Cuba, where it belongs to the Mesozoic basement of the Island. The belt contains three tectonic units: Pino Solo, Mestanza and Cerro de Cabras, each one overthrusted upon the Alturas de Pizarras del Sur unit of the Guaniguanico terrane. This tectono-metamorphic scenario contrasts with the remaining parts of the terrane. The conclusions arrived in this paper are supported by cartographic, petrographic, and structural data, collected during decades, that also includes mineral chemistry content in the micas from the siliciclasts. The clockwise rotation of the main compressive stress &#963;1 developed with singular time-spatial consequences that allow to discriminate several deformational periods (P) from NW 330°-340° up to NE 20°-30° during P1 compression and the development of tectonic transport (P2 and P4). The sinistral Pinar fault (P3) conditioned the birth and tectonic style of the belt from a small change in its trend, provoking transpression in some sector and the development of a positive flower structure (extrusive orogen) and its definite configuration during the last deformation period (P4). In these tectonic conditions occurs some metamorphic processes: mc-very low degree metamorphism, related to cleavage, developed during all periods, mt-transpressive metamorphism of low degree, progressive related to mid pressure-high part (P4 with the highest P/T gradients) and me-metamorphism by tectonic extrusion, of low degree, retrograde with mid pressure-middle part (P4). The juxtaposed emplacement of the extrusive sequences conditioned their metamorphic heterogeneities.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[transpresión]]></kwd>
<kwd lng="es"><![CDATA[extrusión tectónica]]></kwd>
<kwd lng="es"><![CDATA[flor positiva]]></kwd>
<kwd lng="es"><![CDATA[metamorfismo]]></kwd>
<kwd lng="es"><![CDATA[Cuba]]></kwd>
<kwd lng="en"><![CDATA[transpression]]></kwd>
<kwd lng="en"><![CDATA[tectonic extrusión]]></kwd>
<kwd lng="en"><![CDATA[positive flower]]></kwd>
<kwd lng="en"><![CDATA[metamorphism]]></kwd>
<kwd lng="en"><![CDATA[Cuba]]></kwd>
</kwd-group>
</article-meta>
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