<?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>S1026-87742021000100001</article-id>
<article-id pub-id-type="doi">10.22201/cgeo.20072902e.2021.1.1582</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Arreglo de fracturas geológicas en rocas miocénicas de la cuenca de México]]></article-title>
<article-title xml:lang="en"><![CDATA[Geologic fractures arrangement in Miocene rocks from Mexico basin]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Vásquez-Serrano]]></surname>
<given-names><![CDATA[Alberto]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Arce-Saldaña]]></surname>
<given-names><![CDATA[José Luis]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Rangel-Granados]]></surname>
<given-names><![CDATA[Elizabeth]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Morales-Casique]]></surname>
<given-names><![CDATA[Eric]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Arroyo López]]></surname>
<given-names><![CDATA[Sarah María]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad Nacional Autónoma de México Instituto de Geología Departamento de Procesos Litosféricos]]></institution>
<addr-line><![CDATA[Ciudad de México ]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad Nacional Autónoma de México Instituto de Geología Departamento de Dinámica Superficial]]></institution>
<addr-line><![CDATA[Ciudad de México ]]></addr-line>
<country>Mexico</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>00</month>
<year>2021</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>00</month>
<year>2021</year>
</pub-date>
<volume>38</volume>
<numero>1</numero>
<fpage>1</fpage>
<lpage>17</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1026-87742021000100001&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1026-87742021000100001&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1026-87742021000100001&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN El estudio del arreglo de las fracturas es importante para el conocimiento del flujo de fluidos y tiene una amplia aplicación en áreas como: estabilidad de taludes, campos geotérmicos, acuíferos profundos y exploración de hidrocarburos. El arreglo de las fracturas es una característica fundamental de la distribución espacial de las fracturas, aunque su relación con el tipo de roca, fallas kilométricas y herencia estructural es poco conocida. La influencia de estas variables en el arreglo de las fracturas es explorada en este trabajo mediante un estudio detallado de fracturas en rocas miocénicas de la cuenca de México. Las rocas miocénicas en la cuenca de México están afectadas por tres sistemas de fracturas que tienen una orientación NE-SW, NNW-SSE y ~E-W. Las tres familias de fracturas se presentan con un arreglo en forma de grupos de fracturas, donde el grado de agrupamiento está relacionado con el tipo de roca que constituye la sucesión volcánica del Mioceno (lavas y depósitos volcaniclásticos). Adicionalmente, la intensidad de fracturas es mayor en las lavas y menor en los depósitos volcaniclásticos, y tiene una relación inversa con el grado de agrupamiento. La familia F1 (NE-SW) tiene un arreglo de fracturas que se pueden caracterizar con una distribución fractal a escala de metros. Mientras que las fracturas F2 (NNW-SSE) presentan un arreglo que se asocian con anisotropías mecánicas en rocas pre-miocénicas. Este fenómeno probablemente está relacionado con una herencia estructural y/o reactivación de estructuras. Finalmente, las fracturas F3 (~E-W) forman un arreglo que se puede asociar con una distribución espacial aleatoria.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT The study of fracture arrangement is important for the understanding of fluid flow and has a wide application in several areas as slope stability analysis, geothermal fields, deep aquifers and oil exploration. The facture arrangement is an essential characteristic of the spatial distribution of the fractures, although the relation of the spatial arrangement of fractures with variables such as the rock type, the kilometric faults, and structural inheritance is unknowns. We explore de influence of these variables in the facture arrangement through of detail study of Miocene rocks in the Mexico basin. The Miocene rocks in the Mexico Basin are affected by three fracture systems oriented NE-SW, NNW-SSE and ~E-W. All fracture families present a cluster array, where the degree of clustering is related to the rock type that constitute the Miocene volcanic succession (lava flows and volcaniclastic deposits). In addition, the intensity of fracturing is stronger in lava flows than the volcaniclastic deposits, with an inverse relationship to the degree of clustering (Lyapunov Exponent). The F1 family (NE-SW) has groups of fractures characterized by a fractal distribution in mesoscopic scale. Meanwhile, the fractures F2 (NNW-SSE) present groups that are associated with mechanical anisotropy in pre-Miocene rocks. This phenomenon is related to structural inheritance and/or reactivation. Finally, the fractures F3 (~E-W) form groups with a random distribution.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[arreglo de fracturas]]></kwd>
<kwd lng="es"><![CDATA[fractura geológica]]></kwd>
<kwd lng="es"><![CDATA[análisis fractal]]></kwd>
<kwd lng="es"><![CDATA[intensidad de fracturas]]></kwd>
<kwd lng="es"><![CDATA[rocas del Mioceno]]></kwd>
<kwd lng="en"><![CDATA[fracture arrangement]]></kwd>
<kwd lng="en"><![CDATA[geologic fracture]]></kwd>
<kwd lng="en"><![CDATA[fractal análisis]]></kwd>
<kwd lng="en"><![CDATA[fracture intensity]]></kwd>
<kwd lng="en"><![CDATA[Miocene rocks]]></kwd>
</kwd-group>
</article-meta>
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