<?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>0016-7169</journal-id>
<journal-title><![CDATA[Geofísica internacional]]></journal-title>
<abbrev-journal-title><![CDATA[Geofís. Intl]]></abbrev-journal-title>
<issn>0016-7169</issn>
<publisher>
<publisher-name><![CDATA[Universidad Nacional Autónoma de México, Instituto de Geofísica]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S0016-71692015000400323</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[Chapala half-graben structure inferred. A magnetometric study]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Alatorre-Zamora]]></surname>
<given-names><![CDATA[Miguel Angel]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Campos-Enríquez]]></surname>
<given-names><![CDATA[José Oscar]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Rosas-Elguera]]></surname>
<given-names><![CDATA[José Guadalupe]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Peña-García]]></surname>
<given-names><![CDATA[Laura]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Maciel-Flores]]></surname>
<given-names><![CDATA[Roberto]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Fregoso-Becerra]]></surname>
<given-names><![CDATA[Emilia]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad de Guadalajara Departamento de Ingeniería Civil y Topografía ]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad de Guadalajara Departamento de Ciencias Ambientales ]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Universidad de Guadalajara Centro Universitario de los Valles ]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af4">
<institution><![CDATA[,Universidad Nacional Autónoma de México Instituto de Geofísica ]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af5">
<institution><![CDATA[,Universidad de Guadalajara Departamento de Matemáticas ]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
<country>Mexico</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>12</month>
<year>2015</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>12</month>
<year>2015</year>
</pub-date>
<volume>54</volume>
<numero>4</numero>
<fpage>323</fpage>
<lpage>342</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S0016-71692015000400323&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S0016-71692015000400323&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S0016-71692015000400323&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract: Many geologic and tectonic-structural studies refer to the Chapala lake structure in general terms as a graben (or more generally as rift). However, no formal study has addressed its structure. The Chapala Lake is located in a major topographic depression surrounded by broad middle to late Miocene volcaniccapped plateaus. We conducted a magnetic survey comprising five S-N lines crossing the Chapala Lake. One profile comprises a land extension (southwards along roads). Magnetic anomalies obtained are mainly smooth and large scale features associated to the sedimentary infill, local and high amplitude anomalies are due to shallow basaltic and andesitic tilted blocks, and highest amplitudes due to the outcropped basaltic flows of the Los Alacranes and Mezcala islands. The models obtained point to a large structural high located at the central depression portion that separates two structural lows. The structural lows correspond to halfgraben type structures. Through the faults delimiting it were emplaced the basaltic flows of the Mezcala and Los Alacranes islands. The presence of half graben type structures indicates that the crust has been subject to an extensional tectonic.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen: El Lago de Chapala se ubica en una gran depresión topográfica rodeada de amplias me- setas volcánicas del Mioceno medio al tardío. Muchos estudios geológicos y tectónico-estructurales se refieren a la estructura interna de esta depresión topográfica como un graben o genéricamente como rift, aunque su estructura interna no ha sido formalmente establecida. Para este fin se realizó un levantamiento magnético constituido por cinco líneas norte-sur que cruzan al Lago de Chapala. Un perfil se extiende hacia el sur sobre caminos transitables. Las anomalías magnéticas son principalmente suaves y de carácter regional, lo que se debe al relleno sedimentario; anomalías de carácter local son debidas a bloques someros inclinados de composición basáltica y andesítica, y amplitudes altas debidas a flujos de lavas basálticas expuestas en las islas de Los Alacranes y Mezcala. Los modelados indican la presencia de un alto estructural que separa dos bajos estructurales. Los bajos estructurales constituyen estructuras tipo semigraben. A través de las fallas que delimitan este alto estructural se emplazaron los flujos basálticos de las Islas de Los Alacranes y Mezcala. La presencia de estructuras tipo semigraben implican que la corteza ha estado sometida a una tectónica de extensión. Una extensión profunda que adelgazó la corteza podría estar en el origen de las estructuras de tipo semigraben que caracterizan a la depresión Chapala.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[Rift]]></kwd>
<kwd lng="es"><![CDATA[graben]]></kwd>
<kwd lng="es"><![CDATA[semi-graben]]></kwd>
<kwd lng="es"><![CDATA[depresión]]></kwd>
<kwd lng="es"><![CDATA[Lago de Chapala]]></kwd>
<kwd lng="es"><![CDATA[perfiles magnéticos]]></kwd>
<kwd lng="es"><![CDATA[modelado 2D]]></kwd>
<kwd lng="es"><![CDATA[islas basálticas]]></kwd>
<kwd lng="es"><![CDATA[Bloque Michoacán]]></kwd>
<kwd lng="en"><![CDATA[Rift]]></kwd>
<kwd lng="en"><![CDATA[graben]]></kwd>
<kwd lng="en"><![CDATA[half-graben]]></kwd>
<kwd lng="en"><![CDATA[depression]]></kwd>
<kwd lng="en"><![CDATA[Chapala Lake]]></kwd>
<kwd lng="en"><![CDATA[magnetic profiles]]></kwd>
<kwd lng="en"><![CDATA[2D modeling]]></kwd>
<kwd lng="en"><![CDATA[basaltic islands]]></kwd>
<kwd lng="en"><![CDATA[Michoacán Block]]></kwd>
</kwd-group>
</article-meta>
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