<?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>S1405-33222006000100161</article-id>
<article-id pub-id-type="doi">10.18268/bsgm2006v58n1a6</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Características geológicas y potencial metalogenético de los principales complejos ultramáficos-máficos de México]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Ortiz-Hernández]]></surname>
<given-names><![CDATA[Luis Enrique]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Escamilla-Casas]]></surname>
<given-names><![CDATA[José Cruz]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Flores-Castro]]></surname>
<given-names><![CDATA[Kinardo]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Ramírez-Cardona]]></surname>
<given-names><![CDATA[Marius]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Acevedo-Sandoval]]></surname>
<given-names><![CDATA[Otilio]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad Autónoma del Estado de Hidalgo Centro de Investigaciones en Ciencias de la Tierra ]]></institution>
<addr-line><![CDATA[Pachuca Hidalgo]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="Af2">
<institution><![CDATA[,Instituto Politécnico Nacional Unidad Ticomán Sección de Estudios de Posgrado e Investigación, ESIA]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
<country>Mexico</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>00</month>
<year>2006</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>00</month>
<year>2006</year>
</pub-date>
<volume>58</volume>
<numero>1</numero>
<fpage>161</fpage>
<lpage>181</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1405-33222006000100161&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1405-33222006000100161&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1405-33222006000100161&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen El consenso de los principales complejos ultramáficos-máficos (UM-M) en diez estados de la República Mexicana (Baja California, Baja California Sur, Sinaloa, Tamaulipas, Guanajuato, Guerrero, Estado de México, Puebla, Oaxaca y Chiapas) indica que su edad varía entre el Paleozoico y el Paleoceno, y que están asociados a diferentes contextos tectónicos, e. g. raíz de arco volcánico, ofiolita, cuenca oceánica, complejo de subducción y fragmento continental. La mayoría de los complejos UM-M ocurren en los terrenos tectonoestratigráficos Tahué y Náhuatl, y en menor proporción en los terrenos Cochimí, Yuma, Guachichil, Tepehuano, Mixteco, Cuicateco y Maya. Los complejos UM-M más antiguos son los de Cañón del Novillo en Tamaulipas, formado posiblemente en un complejo de subducción. El Fuerte, Agua Caliente y Mazatlán en Sinaloa asociados a cuencas oceánicas (?), y Tehuitzingo-Tecomatlán en Puebla, que corresponde a una ofiolita de tipo zona de suprasubducción. Existen complejos UM-M del Triásico Superior-Jurásico Medio (Isla de Cedros y península de Vizcaíno, e Islas Margarita y Magdalena en Baja California Sur) con afinidad ofiolítica en un complejo de subducción, mientras que los complejos del Cretácico Inferior (Alisitos y Culiacán en Sinaloa, San Juan de Otates en Guanajuato, y Palmar Chico-San Pedro Limón en el Estado de México), son los más característicos y están asociados a las raíces de un arco magmático. Los complejos más recientes son los de Ojos Negros en Baja California (Cretácico Superior-Paleoceno), que representa parte de la raíz plutónica del batolito californiano, y las peridotitas de flogopita con afinidad kimberlítica de San Javier en Sinaloa (Mesozoico superior-Terciario temprano), que están asociadas a un fragmento continental subyacente a un arco magmático. En cuanto a los complejos restantes: Bacubirito, en Sinaloa, está asociado a una ofiolita desmembrada desarrollada en una cuenca oceánica. Cuicatlán-Concepción Pápalo, en Oaxaca, representa posiblemente un arco magmático intracontinental de corta vida. Los complejos UM-M de Guerrero (Las Ollas, Camalotito, Loma Baya y El Tamarindo) se asocian a raíces de arco intraoceánico en un complejo de subducción. Finalmente, los pequeños cuerpos UM-M de Motozintla en Chiapas constituyen fragmentos de la raíz de un arco magmático alojados en una zona de cizalla. Estos complejos UM-M albergan mineralización no metálica desarrollada durante su alteración y/o metamorfismo (asbesto, talco y magnesita), y mineralización metálica producida mediante procesos magmáticos (cuerpos lenticulares alargados o pods de cromitita, diseminaciones de cobre, níquel y cobalto), y pueden contener asimismo trazas de minerales del grupo del platino.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract The consensus of the major mafic-ultramafic complexes (UM-M) in ten states of the Mexican Republic (Baja California, Baja California Sur, Sinaloa, Tamaulipas, Guanajuato, Guerrero, Estado de Mexico, Puebla, Oaxaca, and Chiapas) indicates that their age ranges from Paleozoic to Paleocene and that are associated with diverse tectonic settings: e.g. root volcanic arc, ophiolite, oceanic basin, subduction complex, and continental fragment. The majority of the complexes occur in the following tectonostratigraphic terranes: Tahué and Náhuatl; and in less proportion in Cochimi, Yuma, Guachichil, Tepehuano, Mixteco, Cuicateco and Maya. The older UM-M complexes are: in Tamaulipas, Cañon del Novillo (that probably constitutes a subduction complex); El Fuerte, Agua Caliente, and Mazatlan, in Sinaloa, which are associated with oceanic basins (?); and TehuitzingoTecomatlan, in Puebla, associated with a supra-subduction zone ophiolite. The Late Triassic-Middle Jurassic UM-M complexes (Isla de Cedros, Vizcaino Peninsula, and Isla Margarita and Magdalena in Baja California Sur) have ophiolitic affinity in a subduction complex. Early Cretaceous complexes (Alisitos and Culiacan, in Sinaloa; San Juan de Otates, in Guanajuato; and Palmar Chico-San Pedro Limon, in Estado de Mexico) are the most characteristic and are associated with a dismembered ophiolite developed in an oceanic basin. Among the remainder of the complexes are: Bacubirito, in Sinaloa, associated with a dismembered ophiolite developed in an oceanic basin; Cuicatlan-Concepcion Papalo, in Oaxaca, possibly represents a short living, intracontinental, magmatic arc. The more recent complexes are: Ojos Negros, in Baja California (Late Cretaceous-Paleocene) and corresponds to the plutonic root of the Californian Batholith; and the micaceous peridotites with kimberlitic affinity of San Javier, in Sinaloa (Upper Mesozoic-Early Tertiary) that are associated with a continental fragment underlying a magmatic arc. The UM-M complexes in Guerrero (Las Ollas, Camalotito, Loma Baya y El Tamarindo) are associated with intraoceanic arc roots in a subduction complex. Finally, the small UM-M bodies of Motozintla, in Chiapas, constitute fragments of the root of a magmatic arc allocated in a shear zone. These UM-M complexes host both, non-metallic mineralization developed during alteration and/or metamorphism (asbestos, talc, magnesite) and metallic mineralization produced after magmatic processes (lenticular and elongated bodies, ferrichromite pods, disseminations of copper, nickel, and cobalt) and can also contain traces of platinum group minerals.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[Rocas ultramáficas-máficas]]></kwd>
<kwd lng="es"><![CDATA[características geológicas]]></kwd>
<kwd lng="es"><![CDATA[potencial metalogenético]]></kwd>
<kwd lng="es"><![CDATA[México]]></kwd>
<kwd lng="en"><![CDATA[Ultramafic-mafic rocks]]></kwd>
<kwd lng="en"><![CDATA[Geologic characteristics]]></kwd>
<kwd lng="en"><![CDATA[Metallogenetic potential]]></kwd>
<kwd lng="en"><![CDATA[Mexico]]></kwd>
</kwd-group>
</article-meta>
</front><back>
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