<?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>S1026-87742019000100038</article-id>
<article-id pub-id-type="doi">10.22201/cgeo.20072902e.2019.1.871</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Análisis de fracturas geológicas en el pozo Agrícola Oriental 2C, Ciudad de México y su relación con fallas mayores]]></article-title>
<article-title xml:lang="en"><![CDATA[Analysis of geological fractures in the Agrícola Oriental 2C well, Mexico City, and its relationship with major faults]]></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"/>
<xref ref-type="aff" rid="Aaf"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Camacho-Rangel]]></surname>
<given-names><![CDATA[Rebeca]]></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[Morales-Casique]]></surname>
<given-names><![CDATA[Eric]]></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 Centro de Geociencias ]]></institution>
<addr-line><![CDATA[Juriquilla Querétaro]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Benemérita Universidad Autónoma de Puebla Facultad de Ingeniería Colegio de Geofísica]]></institution>
<addr-line><![CDATA[Ciudad de Puebla Puebla]]></addr-line>
<country>Mexico</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>00</month>
<year>2019</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>00</month>
<year>2019</year>
</pub-date>
<volume>36</volume>
<numero>1</numero>
<fpage>38</fpage>
<lpage>53</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1026-87742019000100038&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1026-87742019000100038&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1026-87742019000100038&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN En años recientes, en la Ciudad de México se han realizado varios pozos exploratorios de hasta 2000 m de profundidad, con el fin de encontrar acuíferos que ayuden a disminuir el desabasto de agua potable para el área metropolitana. En particular, en el pozo Agrícola Oriental 2C, perforado en la Alcaldía de Iztacalco, se recuperaron varios núcleos, uno de los cuales mide 9 m, ubicado entre 1550 y 1559 m de profundidad, cercano al contacto entre rocas calcáreas del Cretácico y rocas volcánicas del Oligoceno, a ~1560 m de profundidad. El núcleo muestra que las rocas volcánicas se encuentran afectadas por una cantidad importante de fracturas, las cuales pueden ser divididas en dos familias con base en su relleno y relaciones de corte (F1 y F2). Las fracturas más jóvenes (F2) se relacionan con una falla, llamada informalmente en este trabajo falla Agrícola Oriental, que pone en contacto rocas sedimentarias y volcánicas. Las fracturas fueron caracterizadas mediante un análisis detallado de la cantidad, geometría y distribución a lo largo de una línea de muestreo, tomando en cuenta ambas familias de fracturas. Estas variables fueron expresadas en términos de intensidad de fracturas, dimensión fractal de caja y correlación, exponente de Lyapunov, coeficiente de variación y exponente de frecuencia acumulada. Los resultados obtenidos muestran que el espaciamiento entre fracturas, así como la apertura, se ajustan muy bien a una ley de potencia en un gráfico bilogarítmico de su frecuencia acumulada, por lo que las fracturas exhiben un comportamiento fractal. El valor de la intensidad de fracturas, dimensión fractal, exponente de Lyapunov y exponente de frecuencia acumulada de la apertura, disminuyen progresivamente con el aumento de la distancia a la falla, mientras que el coeficiente de variación y exponente de frecuencia acumulada del espaciamiento presentan un patrón contrario. Estos comportamientos suelen ser típicos en una zona de cizalla común, sin embargo, un aspecto importante encontrado en este estudio es la alteración de estos patrones con la presencia de un grupo de fracturas preexistentes (F1) a la formación de un nuevo grupo de fracturas (F2), lo cual provoca un aumento en la cantidad de fracturas y una redistribución de estas estructuras dentro de la zona de falla. Adicionalmente, con base en las características de las fracturas estudiadas, se propone que la falla encontrada en este estudio pertenece al sector norte de la fosa de Santa Catarina y tiene una orientación ENE-WSW.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT In the last years several exploratory wells have been drilled in Mexico City down to 2000 m depth, with the aim to explore deep aquifers to cover the water deficiency in the metropolitan area. In particular, in the Agricola Oriental 2C well, located in the Iztacalco municipality, several cores were recovered; one of them is 9 m long, located between 1550 and 1559 m depth. This core is situated close to the contact between an Oligocene volcanic unit and a Cretaceous limestone at ~1560 m depth. The study core shows that the volcanic rocks are affected by an important number of fractures, which can be divided into two families according to their intersection relationships and fill material (F1 and F2). The younger fractures (F2) are related with a fault, informally named here as Agricola Oriental fault, which sets in tectonic contact the sedimentary and the volcanic rocks. The fractures were characterized through a detailed analysis of their number, geometry and spatial arrangement, using the scan line method and taking into account both families of fractures. These variables were expressed such as fracture intensity, box and correlation fractal dimensions, Lyapunov exponent, variation coefficient, and cumulative frequency exponent. Our results show that the spacing between fractures and the aperturefollow a power law in a log-log graph of the cumulative frequency analysis that results in a fractal behavior. The pattern values showed in the fracture intensity, fractal dimension, Lyapunov exponent, and aperture cumulative frequency exponent progressively diminish as the distance to the fault increases. In turn, the coefficients of variation and spacing cumulative frequency exponent have a different pattern: their values increase with the distance to the fault. These behaviors are typical of a common shear zone; however, in our analysis, the anomalous variation of the study parameters in the fault damaged zone is related to the presence of a previous fracture system (F1). These fractures induced an important increase in the amount of fractures and change their distribution in the damage zone. In addition, based on the fracture characteristics, we proposed that the fault found in the well is related to the northern limit of Santa Catarina graben and has an ENE-WSW orientation.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[fractura geológica]]></kwd>
<kwd lng="es"><![CDATA[análisis fractal]]></kwd>
<kwd lng="es"><![CDATA[arreglo de fracturas]]></kwd>
<kwd lng="es"><![CDATA[intensidad de fracturas]]></kwd>
<kwd lng="es"><![CDATA[falla Agrícola Oriental]]></kwd>
<kwd lng="en"><![CDATA[fracture]]></kwd>
<kwd lng="en"><![CDATA[fractal analysis]]></kwd>
<kwd lng="en"><![CDATA[fracture array]]></kwd>
<kwd lng="en"><![CDATA[fracture intensity]]></kwd>
<kwd lng="en"><![CDATA[Agrícola Oriental Fault]]></kwd>
</kwd-group>
</article-meta>
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