<?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>S1405-33222005000100083</article-id>
<article-id pub-id-type="doi">10.18268/bsgm2005v57n1a5</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[La falla de Caltepec: raíces expuestas de una frontera tectónica de larga vida entre dos terrenos continentales del sur de México]]></article-title>
<article-title xml:lang="en"><![CDATA[The Caltepec fault: exposed roots of a long-lived tectonic boundary between two continental terranes of southern Mexico]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Elías-Herrera]]></surname>
<given-names><![CDATA[Mariano]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Ortega-Gutiérrez]]></surname>
<given-names><![CDATA[Fernando]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Sánchez-Zavala]]></surname>
<given-names><![CDATA[José Luis]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Macías-Romo]]></surname>
<given-names><![CDATA[Consuelo]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Ortega-Rivera]]></surname>
<given-names><![CDATA[Amabel]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Iriondo]]></surname>
<given-names><![CDATA[Alexander]]></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 ]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Universidad Nacional Autónoma de México Instituto de Geología Estación Regional del Noroeste]]></institution>
<addr-line><![CDATA[Hermosillo ]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af3">
<institution><![CDATA[,Universidad Nacional Autónoma de México Centro de Geociencias ]]></institution>
<addr-line><![CDATA[Querétaro Qro.]]></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>83</fpage>
<lpage>109</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1405-33222005000100083&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1405-33222005000100083&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1405-33222005000100083&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen En este trabajo se discuten las características geológicas de la falla de Caltepec, una zona de cizalla de larga vida con dirección norte-sur y mecanismo transpresional derecho que separa a los terrenos Zapoteco al oriente y Mixteco al poniente al nivel de sus basamentos metamórficos (complejos Oaxaqueño y Acatlán). Los excelentes afloramientos (área de Caltepec) que exponen completamente el contacto en una anchura variable entre 2 y 6 km revelan una actividad tectonomagmática y metamórfica del Pérmico temprano relacionada con la yuxtaposición de los complejos cristalinos durante la consolidación de Pangea, y registran también períodos múltiples de reactivación mesozoicos, cenozoicos y probablemente hasta recientes. Con base en la cartografía geológico-estructural detallada y estudios petrográficos, geocronológicos e isotópicos, se determinó un rango de edad de 275.6&#8722;270.4 Ma para el evento de cizalla dúctil en la zona de falla mediante fechamientos U-Pb en circones de un leucosoma anatéctico y granito sintectónico (granito Cozahuico). Se establece también una estructura en semiflor con su cima en posición casi vertical y su base cabalgada hacia el poniente con desplazamientos indeterminados. Las relaciones iniciales de 87Sr/86Sr (0.70435-0.70686) y edades modelo Sm-Nd (TDM) (1.0-1.6 Ga) para el granito Cozahuico y el leucosoma indican un origen por mezcla magmática entre corteza local proterozoica y una componente de manto empobrecido. La edad leonardiana de la cobertura discordante (Formación Matzitzi) y una edad de enfriamiento 40Ar/39Ar (moscovita) de 268.6 Ma para un esquisto de mica milonítico en la base de la cabalgadura, implica tasas altas de enfriamiento (~180°C/Ma) y levantamiento durante el Pérmico. Por otro lado, el registro sedimentológico adyacente indica reactivación tectónica intensa durante el Cretácico Inferior, Paleógeno y Neógeno a lo largo de la falla de Caltepec, alternando con periodos de estabilidad tectónica relativa durante el Triásico, Jurásico y Cretácico medio. La orientación paralela de las fallas de Caltepec y Oaxaca, distante decenas de kilómetros al oriente de la primera, se interpreta como partes de un sistema estructural sincrónico y dinámicamente acoplado que ha estado liberando alternadamente los esfuerzos tectónicos asociados con la ruptura de Pangea y la evolución del margen del Pacífico del sur de México desde el Jurásico hasta el Holoceno en esta región.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract This work presents the main geologic characteristics of the long-lived Caltepec fault zone, a N-S trending, righttranspressional shear zone that separates the Zapoteco terrane on the east from the Mixteco terrane on the west at their basement level (Oaxaqueño and Acatlan complexes). The high quality of the outcrops (Caltepec area), entirely exposing a 2-6 km wide tectonic contact, reveals protracted and polyphase tectonic activity on the fault from at least early Permian time to the present. Based on detailed geological mapping, petrography, geochronology, and isotopic studies, it is shown that the tectonothermal event in the Caltepec fault zone is related to the oblique collision of the metamorphic complexes during the amalgamation of Pangea. An anatectic leucosome and the resulting syntectonic granite (Cozahuico granite) in the fault zone yielded U-Pb zircon ages of 275.6 and 270.4 Ma. It is also established a half-flower structure for the fault zone, with the top lying almost vertical and its base thrusted westward with unknown displacements. The initial 87Sr/86Sr ratios (0.70435-0.70686) and Sm-Nd model ages (TDM) (1.0-1.6 Ga) for the Cozahuico granite and leucosome indicate a magmatic mixture that originated from melted Proterozoic crust and a component of depleted mantle. The leonardian age for the cover (Matzitzi Fm.) and a 40Ar/39Ar cooling age (muscovite) of 268.6 Ma for a mylonitic mica schist at the sole of the thrust, implies high ratios of cooling (~180°C/Ma) and uplift during the Permian. On the other hand, the adjacent sedimentological record indicates intense tectonic reactivation during Early Cretaceous, Paleogene, and Neogene times along the long-lived Caltepec fault zone, alternating with periods of relative tectonic quiescence during Triassic, Jurassic, and mid Cretaceous times. The trend of the Caltepec fault zone, parallel to the Oaxaca fault, distant only a few kilometers to the east, is interpreted as part of a synchronous and dynamically coupled tectonic system. This coupled system has liberated tectonic stresses associated with the rupture of Pangea and the evolution of the Pacific margin of southern Mexico from Jurassic to Holocene times.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[Falla mayor]]></kwd>
<kwd lng="es"><![CDATA[límite de terrenos]]></kwd>
<kwd lng="es"><![CDATA[Complejo Acatlán]]></kwd>
<kwd lng="es"><![CDATA[Complejo Oaxaqueño]]></kwd>
<kwd lng="es"><![CDATA[México meridional]]></kwd>
<kwd lng="en"><![CDATA[Major fault]]></kwd>
<kwd lng="en"><![CDATA[terrane boundary]]></kwd>
<kwd lng="en"><![CDATA[Acatlán Complex]]></kwd>
<kwd lng="en"><![CDATA[Oaxacan Complex]]></kwd>
<kwd lng="en"><![CDATA[southern Mexico]]></kwd>
</kwd-group>
</article-meta>
</front><back>
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