<?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>S1026-87742023000100016</article-id>
<article-id pub-id-type="doi">10.22201/cgeo.20072902e.2023.1.1716</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Control estructural de mineralizaciones por dilatancias debido a expansividad térmica diferencial (en depósitos diseminados) y flexiones de fallas (en venas): revisión e hipótesis de trabajo]]></article-title>
<article-title xml:lang="en"><![CDATA[The structural control of mineralizations by dilatancies due to differential thermal expansivity (in disseminated deposits) and faults bending (in veins): revision and working hypothesis]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Rossello]]></surname>
<given-names><![CDATA[Eduardo Antonio]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[López-Isaza]]></surname>
<given-names><![CDATA[Julián Andrés]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad de Buenos Aires  ]]></institution>
<addr-line><![CDATA[ Buenos Aires]]></addr-line>
<country>Argentina</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Servicio Geológico Colombiano  ]]></institution>
<addr-line><![CDATA[ Bogotá]]></addr-line>
<country>Colombia</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>00</month>
<year>2023</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>00</month>
<year>2023</year>
</pub-date>
<volume>40</volume>
<numero>1</numero>
<fpage>16</fpage>
<lpage>34</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1026-87742023000100016&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1026-87742023000100016&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1026-87742023000100016&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN La generación de espacios dilatantes en las rocas hospedantes es fundamental para facilitar la circulación y acumulación de fluidos mineralizantes con potencial económico. En depósitos diseminados, los cambios volumétricos y morfológicos en rocas con cuarzo y feldespato, debido a sus coeficientes de dilatación (contracción) térmica diferencial relativa, determinan dilatancia haciéndolos porosos y permeables a los fluidos. Las constantes de dilatación térmica contrastantes para el cuarzo y el feldespato en procesos termocrecientes y termodecrecientes se revisan mediante el modelado volumétrico del efecto de una variación significativa de la transición de cuarzo &#945;&#8722;&#946; alrededor de 575 °C. Este fenómeno podría variar desde 0.4 % para un granitoide con bajo contenido de cuarzo hasta 1.2 % durante el enfriamiento de un boxwork porfírico típico. En el caso de cuerpos vetiformes, el fallamiento produce dilatación por flexión transtensiva con aumento de su influencia cuando muestran formas irregulares, escalonadas o flexuradas. De acuerdo con la Ley de Anderson, las porciones de estas fallas serán dilatantes cuando el ángulo con el esfuerzo principal compresivo subparalelo (&#947; = ángulo entre &#963;1 y la superficie de falla) es pequeño. El conocimiento morfoestructural y cinemático de los mecanismos generadores de dilatancia controlante de las mineralizaciones constituye una valiosa y práctica metodología de trabajo, que contribuye al pronóstico de localización de los mejores sectores de mineralización en volumen y calidad durante las actividades de prospección y exploración. Ambos mecanismos físicos que generan la dilatancia en las rocas huésped son factores de suma importancia en la definición económica de las mineralizaciones que las ocupan.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT The generation of dilating spaces in the host rocks is essential to facilitate the circulation and accumulation of mineralizing fluids with economic potential. In disseminated deposits, the volumetric and morphological changes in rocks with quartz and feldspar, due to their coefficients of relative differential thermal expansion (contraction), determine dilatancy, making them porous and permeable to fluids. The contrasting thermal expansion constants for quartz and feldspar in thermo-increasing and thermo-decreasing processes are reviewed by volumetric modeling of the effect of a significant variation of the quartz transition &#945;&#8722;&#946; around 575 °C. This phenomenon could vary from 0.4 % to 1.2 % for granite with different quartz content during the cooling of a typical porphyry boxwork. In the case of vein bodies, faulting produces dilation by transtensive bending with an increase in thickness when they show irregular, stepped and/or bended shapes. According to Anderson&amp;apos;s Law, portions of these faults will be dilatant when the principal stresses are subparallel (&#947; = the angle between &#963;1 and the fault surface). The morphostructural and kinematic knowledge of the mechanisms that generate the controlling dilatancy of mineralization constitutes a valuable and practical work methodology that contributes to the location forecast of the best mineralization sectors in terms of volume and quality during prospecting and exploration activities. Both described physical mechanisms that generate dilation in the host rocks are factors of great importance in the economic definition of the mineralizations control.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[expansión térmica]]></kwd>
<kwd lng="es"><![CDATA[control estructural]]></kwd>
<kwd lng="es"><![CDATA[cuarzo &#945;&#8722;&#946;]]></kwd>
<kwd lng="es"><![CDATA[emplazamiento de menas]]></kwd>
<kwd lng="es"><![CDATA[fracturas]]></kwd>
<kwd lng="en"><![CDATA[thermal expansion]]></kwd>
<kwd lng="en"><![CDATA[structural control]]></kwd>
<kwd lng="en"><![CDATA[&#945;&#8722;&#946; quartz]]></kwd>
<kwd lng="en"><![CDATA[ore emplacement]]></kwd>
<kwd lng="en"><![CDATA[fractures]]></kwd>
</kwd-group>
</article-meta>
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