<?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>S0016-71692005000200197</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[Paleomagnetic reconstruction of Coahuila, Mexico: the Late Triassic Acatita intrusives]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Molina Garza]]></surname>
<given-names><![CDATA[Roberto S.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad Nacional Autónoma de México Campus Juriquilla Centro de Geociencias]]></institution>
<addr-line><![CDATA[Querétaro ]]></addr-line>
<country>Mexico</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>06</month>
<year>2005</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>06</month>
<year>2005</year>
</pub-date>
<volume>44</volume>
<numero>2</numero>
<fpage>197</fpage>
<lpage>210</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S0016-71692005000200197&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S0016-71692005000200197&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S0016-71692005000200197&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="en"><p><![CDATA[ABSTRACT The Acatita plutons intrude the upper Paleozoic of Las Delicias, southern Coahuila. We collected 96 samples from 15 sites in two plutons from Valle El Sobaco and Sierra Los Remedios for paleomagnetic and 40Ar-39Ar analyses. Separates of hornblende (215.9 ±1.9 Ma, 2a confidence level), biotite (217.3 ±1.2 Ma), and K-feldspar (205.6 ±1.4 Ma) yield nearly flat age spectra although none of the data satisfy strict plateau criteria, possibly reflecting slight alteration. The preferred ages are interpreted as fairly precise records of Late Triassic cooling of the plutonic suite, which has yielded concordant U-Pb Zircon ages ca. 220 Ma. Most samples yield north-directed and steep positive magnetizations similar to the late Cenozoic expected field direction. Some samples, mostly from mafic enclaves, show northwest magnetization of shallow inclination (southeast at one site) with alternating fields above ~30 mT and thermal demagnetization above ~400°C. The overall mean direction, corrected for 15° northeast dip of the overlying lower Cretaceous strata (dec=342.7°, inc=+4.2°; k=35.4, a95=9.4°, n=8 sites) indicates moderate counterclockwise (14°±8°) rotation with respect to the Late Triassic cratonic reference (reference pole: 57.5°N / 84°E), and moderate southward displacement (7°±5°). The Acatita pole falls within a cluster of Late Triassic poles from Africa, South America, and North America as restored in North American coordinates. A major difficulty is distinguishing local, small-scale rotations, such as a gentle tilt of the pluton after magnetization, from regional events involving large-scale displacements. Rotations such as observed at Acatita are suggested by synfolding magnetizations (Eocene in age) in the transverse sector of the Sierra Madre Oriental and by primary magnetizations in Eocene volcanic rocks near Chihuahua. Therefore rotations of Coahuila Island may be a Cenozoic attribute related to late Laramide deformation. Reconstructions of western equatorial Pangea should place the Coahuiltecano terrane at or near its present position with respect to North America.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[RESUMEN La serie plutónica de Acatita intrusiona estratos del Paleozoico superior de la secuencia de la cuenca Las Delicias, en la porción sur de la plataforma de Coahuila, en el norte de México. Obtuvimos 96 muestras (15 sitios) de dos intrusivos en localidades en el valle el Sobaco y la Sierra de los Remedios para estudios paleomagnéticos y geocronología de 40Ar-39Ar. Separados de hornblenda (215.9 ±1.9 Ma, nivel de confianza 2a), biotita (217.3 ±1.2 Ma) y feldespato potásico (205.6 ±1.4 Ma) producen espectros de emisión de argón casi planos, pero ninguno de ellos satisface criterios estrictos de meseta, posiblemente reflejando algo de alteración. Las edades, sin embargo, son interpretadas como registros relativamente precisos de enfriamiento en el Triásico tardío de la serie plutónica, de la que se han reportado edades concordantes en zircones ca. 220 Ma por el método U-Pb. La mayoría de las muestras contienen magnetizaciones dirigidas hacia el norte y con inclinaciones moderadas positivas, similares a la dirección del campo magnético esperada en el Cenozoico tardío. No obstante, las trayectorias de desmagnetización no están dirigidas hacia el origen y en un número reducido de muestras, obtenidas principalmente en enclaves máficos, se obtuvo una dirección característica dirigida hacia el noroeste y de inclinación casi horizontal (hacia el sureste en un sitio interpretado como polaridad reversa). La magnetización se identifica después de aplicar campos alternos de ~30 mT o temperaturas arriba de los 400°C. La dirección media, corregida por el leve basculamiento (~15°) hacia el noreste de estratos del Cretácico que sobreyacen a los intrusivos es de dec=342.7°, inc=+4.2° (k=35.4, a95=9.4°, n=8 sitios) e indica una rotación anti-horaria (14°±8°) con respecto a la dirección esperada utilizando el polo de referencia de Norte América del Triásico tardío (57.5°N/84°E). También indica un pequeño desplazamiento latitudinal (7°±5°). El polo para Acatita se localiza asociado a un grupo de polos del Triásico tardío para África, Sud-América y Norte América rotados en coordenadas para Norte América. Uno de los principales obstáculos para interpretar los datos de terrenos que conforman hoy México es distinguir efectos de deformación local, como basculamiento de los intrusivos después del enfriamiento, de efectos regionales que involucran grandes desplazamientos. Rotaciones de magnitud similar y en el mismo sentido que la observada en Acatita se han observado en magnetizaciones secundarias (de edad Eoceno), sin-plegamiento, en el sector transversal de la Sierra Madre Oriental, así como en direcciones primarias en rocas volcánicas cerca de Chihuahua. Por ello, interpretamos la rotación de la paleoisla de Coahuila como un atributo Cenozoico asociado a la deformación Laramídica que afecta la región. Utilizando los datos paleomagnéticos para Coahuila y datos publicados para la región, proponemos que reconstrucciones paleogeográficas de la región ecuatorial occidental de Pangea deben reconstruir al terreno Coahuiltecano en o cerca de su posición actual con respecto a Norte América.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[Paleomagnetismo]]></kwd>
<kwd lng="es"><![CDATA[Coahuila]]></kwd>
<kwd lng="es"><![CDATA[México]]></kwd>
<kwd lng="es"><![CDATA[Triásico tardío]]></kwd>
<kwd lng="es"><![CDATA[Pangea]]></kwd>
<kwd lng="en"><![CDATA[Paleomagnetism]]></kwd>
<kwd lng="en"><![CDATA[Mexico]]></kwd>
<kwd lng="en"><![CDATA[Coahuila]]></kwd>
<kwd lng="en"><![CDATA[Late Triassic]]></kwd>
<kwd lng="en"><![CDATA[Pangea]]></kwd>
</kwd-group>
</article-meta>
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