<?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>1405-3322</journal-id>
<journal-title><![CDATA[Boletín de la Sociedad Geológica Mexicana]]></journal-title>
<abbrev-journal-title><![CDATA[Bol. Soc. Geol. Mex]]></abbrev-journal-title>
<issn>1405-3322</issn>
<publisher>
<publisher-name><![CDATA[Sociedad Geológica Mexicana A.C.]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S1405-33222005000100111</article-id>
<article-id pub-id-type="doi">10.18268/bsgm2005v57n1a6</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[La falla Chacalapa en el sur de Oaxaca]]></article-title>
<article-title xml:lang="en"><![CDATA[The Chacalapa fault in southern Oaxaca]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Tolson]]></surname>
<given-names><![CDATA[Gustavo]]></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 Geología Regional]]></institution>
<addr-line><![CDATA[México ]]></addr-line>
<country>Mexico</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>00</month>
<year>2005</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>00</month>
<year>2005</year>
</pub-date>
<volume>57</volume>
<numero>1</numero>
<fpage>111</fpage>
<lpage>122</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1405-33222005000100111&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1405-33222005000100111&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1405-33222005000100111&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen A lo largo de la costa de Oaxaca, entre Puerto Ángel y Santiago Astata, afloran rocas metamórficas del Complejo Xolapa intrusionadas por rocas ígneas de edad Paleógeno a Mioceno sin metamorfismo regional. Ambas unidades se encuentran en contacto tectónico a lo largo de zonas de cizalla con rocas proterozoicas del Complejo Oaxaqueño al norte de Pochutla y con rocas sedimentarias mesozoicas discordantes que sobreyacen los gneises. La principal de estas zonas de cizalla en el área de estudio es la falla Chacalapa, expuesta al norte de Pochutla, que está constituida por ultramilonitas, milonitas, protomilonitas, pseudotaquilitas, filonitas y cataclasitas en orden cronológico de desarrollo. La cinemática de esta zona de cizalla vertical es predominantemente lateral-izquierda. Las rocas miloníticas de la falla Chacalapa registran temperaturas de recristalización dinámica de ~500°C (deformación cristal-plástica de feldespatos) que disminuyen sistemáticamente hasta el régimen netamente quebradizo. Asociadas a la recristalización dinámica se desarrollaron texturas cristalográficas de cuarzo en las rocas miloníticas que, cuando son asimétricas, exhiben un sentido de cizalla izquierdo. Las rocas del régimen quebradizo también registran una cinemática izquierda, al igual que las fallas activas. La edad de las rocas miloníticas de la falla Chacalapa se ubica entre los 29±0.2 y los 23.7±1.2 Ma. El límite de edad superior lo constituye la edad del intrusivo Huatulco (U-Pb de circones, Herrmann et al. 1994) que se observa milonitizado en su margen septentrional y el límite de edad inferior corresponde a la edad K-Ar de hornblenda procedente de diques granodioríticos porfídicos que truncan la milonita.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract Along the coast of Oaxaca between Puerto Angel and Santiago Astata a suite of rocks is exposed corresponding to the Xolapa metamorphic complex which is intruded by granitoid igneous rocks of Paleogene to Miocene age. Both of these rock units are in fault-contact along coast-parallel shear zones with granulite facies metamorphic rocks of the proterozoic age Oaxaca Complex and with cover rocks which unconformably overlie this crystalline basement. The largest of these shear zones is the Chacalapa shear zone exposed to the north of the town of Pochutla and formed by ultramylonites, mylonites, protomylonites, pseudotachylites, phyllonites and cataclasites. The kinematics of this shear zone are dominantly left-lateral. The mylonitic rocks of the Chacalapa shear zone indícate temperatures ~500°C (as evidenced by crystal-plastic deformation of plagioclase feldspar) which decrease systematically to a strictly brittle deformation regime. Quartz crystallographic textures associated with crystal-plastic deformation processes are locally asymmetric, indicating left-lateral shear. Brittle structures also exhibit left-lateral shear-sense indicators, as do active deformation structures. The age of the shear zone is constrained between 29±0.2 and 23.7±1.2 Ma. The upper limit is the age of the Huatulco granodiorite (U-Pb from zircon, Herrmann et al. 1994), whose northern contact is sheared, and the lower bound is fixed by the K-Ar age of hornblende separatedfrom granodioritic dikes which cut the mylonitic lineation.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[Falla]]></kwd>
<kwd lng="es"><![CDATA[México]]></kwd>
<kwd lng="es"><![CDATA[Oaxaca]]></kwd>
<kwd lng="es"><![CDATA[milonita]]></kwd>
<kwd lng="es"><![CDATA[pseudotaquilita]]></kwd>
<kwd lng="es"><![CDATA[Xolapa]]></kwd>
<kwd lng="en"><![CDATA[Fault]]></kwd>
<kwd lng="en"><![CDATA[Mexico]]></kwd>
<kwd lng="en"><![CDATA[Oaxaca]]></kwd>
<kwd lng="en"><![CDATA[mylonite]]></kwd>
<kwd lng="en"><![CDATA[pseudotachylite]]></kwd>
<kwd lng="en"><![CDATA[Xolapa]]></kwd>
</kwd-group>
</article-meta>
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