<?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>S1026-87742021000300226</article-id>
<article-id pub-id-type="doi">10.22201/cgeo.20072902e.2021.3.1669</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Deformación frágil en rocas del Mioceno de la región Morelia-Cuitzeo, Michoacán: implicaciones en el sistema geotérmico local]]></article-title>
<article-title xml:lang="en"><![CDATA[Brittle deformation in Miocene rocks of the Morelia-Cuitzeo region, Michoacán: implications on the local geothermal system]]></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[Rangel-Granados]]></surname>
<given-names><![CDATA[Elizabeth]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Garduño-Monroy]]></surname>
<given-names><![CDATA[Víctor Hugo]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Bermejo Santoyo]]></surname>
<given-names><![CDATA[Gerardo]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Jiménez-Haro]]></surname>
<given-names><![CDATA[Adrián]]></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 Michoacana de San Nicolás Hidalgo Instituto de Investigaciones Metalúrgicas Cuerpo Académico Consolidado de Ciencias de la Tierra]]></institution>
<addr-line><![CDATA[Morelia Michoacán]]></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>3</numero>
<fpage>226</fpage>
<lpage>238</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1026-87742021000300226&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1026-87742021000300226&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1026-87742021000300226&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen La deformación frágil se relaciona con la presencia de fallas y fracturas que afectan a la corteza superior de la Tierra. La distribución que tiene la deformación frágil y el arreglo que presentan las fallas y fracturas son variables poco conocidas, a pesar de que tienen una gran influencia en la generación de permeabilidad y son importantes para entender fenómenos como la deformación localizada. En este trabajo se explora la distribución de la deformación frágil y el arreglo de las fracturas que afectan a rocas andesíticas del Mioceno en el área de Morelia-Cuitzeo mediante un análisis cuantitativo de la deformación a escala mesoscópica. Las rocas miocénicas del área de estudio están afectadas por dos familias de fracturas (F1 y F2) relacionadas con dos eventos de deformación frágil (D1 y D2) ocurridos entre el Mioceno y el Holoceno. Las fracturas F1 tienen un rumbo preferencial NNW-SSE y acomodan una extensión ENE-WSW de ~2.5 %. Por otro lado, las fracturas F2 cortan a las fracturas F1, tienen un rumbo ENE-WSW y se relacionan con una extensión ~N-S de 6.8 %. Ambas familias de fracturas tienen un arreglo de fracturas agrupadas y una intensidad de fracturas promedio similar de aproximadamente 17 fracturas/ metro. Este comportamiento en la intensidad de fracturas, ante una cantidad de deformación por extensión distinta, se atribuye al tipo de roca. La cantidad de extensión asociada a las dos familias de fracturas se distribuye de manera heterogénea en las rocas, lo que contribuye de manera significativa con la porosidad secundaria (porosidad de fracturas). Adicionalmente, la cantidad y el arreglo de las fracturas sugieren que las rocas miocénicas pueden ser la capa permeable del sistema geotérmico de la zona del lago de Cuitzeo.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract Brittle deformation is accommodated by faults and fractures, which affect the upper crust of the Earth. The distribution of brittle deformation and the arrangement of faults and fractures are little known variables, although they influence the rock permeability and are important to understand the strain concentration. Our work explores the strain distribution and the fault arrangement on Miocene andesitic rocks in the Morelia-Cuitzeo area through a quantitative strain analysis at the mesoscopic scale. Two fracture families (F1 and F2) affect the rocks in the study area, and they are related to two brittle deformation events (D1 and D2) occurred between the Miocene and the Recent. The F1 fractures have an NNW-SSE strike and accommodate ~2.5 % of a ENE-WSW extension. The F2 fractures cut the F1 fractures, have an ENE-WSW strike, and accommodate ~7 % of a ~N-S extension. Both facture families have an arrangement of fracture clusters and average fracture intensity of 17 fractures/meter. The fracture intensity behavior is related to the rock type and not to the amount of strain. The finite strain (extension) of the F1 and F2 fractures has a heterogeneous distribution. This behavior contributes significantly to secondary porosity associated with F1 and F2 fractures. The strain distribution, and the quantity and arrangement of the fractures suggest that the Miocene rocks may be the permeable package of a geothermal system in the Cuitzeo Lake area.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[deformación frágil]]></kwd>
<kwd lng="es"><![CDATA[fallas]]></kwd>
<kwd lng="es"><![CDATA[fracturas]]></kwd>
<kwd lng="es"><![CDATA[arreglo de fracturas]]></kwd>
<kwd lng="es"><![CDATA[fractal]]></kwd>
<kwd lng="es"><![CDATA[México]]></kwd>
<kwd lng="en"><![CDATA[fragile deformation]]></kwd>
<kwd lng="en"><![CDATA[faults]]></kwd>
<kwd lng="en"><![CDATA[fractures]]></kwd>
<kwd lng="en"><![CDATA[arrangement of fractures]]></kwd>
<kwd lng="en"><![CDATA[fractal]]></kwd>
<kwd lng="en"><![CDATA[Mexico]]></kwd>
</kwd-group>
</article-meta>
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