<?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>1405-7743</journal-id>
<journal-title><![CDATA[Ingeniería, investigación y tecnología]]></journal-title>
<abbrev-journal-title><![CDATA[Ing. invest. y tecnol.]]></abbrev-journal-title>
<issn>1405-7743</issn>
<publisher>
<publisher-name><![CDATA[Universidad Nacional Autónoma de México, Facultad de Ingeniería]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S1405-77432005000100019</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Neotectónica y facies sedimentarias cuaternarias en el suroeste del Golfo de México, dentro del marco tectono-estratigráfico regional evolutivo del Sur de México]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Aguayo-Camargo]]></surname>
<given-names><![CDATA[J.E.]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,UNAM Facultad de Ingeniería ]]></institution>
<addr-line><![CDATA[ ]]></addr-line>
<country>Mexico</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>03</month>
<year>2005</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>03</month>
<year>2005</year>
</pub-date>
<volume>6</volume>
<numero>1</numero>
<fpage>19</fpage>
<lpage>45</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1405-77432005000100019&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1405-77432005000100019&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1405-77432005000100019&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[Abstract The studied area comprises the south western Gulf of Mexico and the external margin of the south eastern coastal plain of Mexico, with an extensión of 150 000 km2. The geo logical province resulted from the intermittent movements of five major tectonic plates through space and time: Northamerica plate (1); the circum-pacific plates: Kula (2), Farallon (3) and Cocos (5), and the Caribbean plate (5). Due to these cortical movements, 12 to 14 km of sedimentary column were de posited in the marginal continental accretionary prism in environments which varied from continental to deep marin, since Late Triassic trough Recent. Based on the geological and geophysical data from the marine and continental sub surface facilited by Pemex-IMP; such in formation was intergrated with the one previously established by several authors, from the out crop ping stratigraphic sequences of the Sierra de Chiapas, which were verified at selected lo calities, and also with the Quaternary data obtained during this research, with all these data it is here in interpreted the following stratigraphic mega sequences at south eastern Mexico and south western Gulf of Mexico: 1) Mesozoic transgression, 2) Paleogene regression, 3) Neo-generegression, 4) Pleistocene-late Holoceneregression and transgression, and 5) eustaticstability since late Holocene. At the studied area morpho-bathymetry map of the sea floor by means of a continuous linear hydro-acoustic sounder of the R/V &#8220;Justo Sierra&#8221; owned by UNAM. In this map, most prominent fault systems and salt diapirs out cropping on the sea floor make conspicuous, this data was complemented with that from the stratigraphic wells and seis mic-stratigraphy profiles from the subsurface marine provinces provided by Pemex-IMP. It is here in interpreted with the integrated information, the clockwise rotation of the Yucatan block which moves in its south ernportion in Central America, along the geological province of the Libertad Arch and of the Polochic left-lateral fault ing system. The clockwise tectonic movements of the Yucatan microplate were specially important during late Miocene-early Pliocene, because it caused the reactivation and subsidence of the Tertiary tensional basins of Macuspana, Comalcalco and Salina del Istmo at south eastern Mexico.]]></p></abstract>
<abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen El área de estudio se ubica en la porción Sur-Occidental del Golfo de México y en el margen externo de la llanura costera del Sureste de México, con una extensión de unos 150 000 km2. Esta provincia geológica es resultado de los movimientos tectónicos intermitentes, espacio-temporales, de cinco placas tectónicas mayores: la de Norteamérica (1); las circum-pacíficas: Kula (2), Farallón (3) y Cocos (4), así como la del Caribe (5). Debido a los movimientos corticales referidos, en el prisma acrecional marginal continental del Golfo de México se acumularon intermitentemente, entre 12 y 14 km de espesores máximos de sedimentos en ambientes, desde continentales hasta marinos profundos durante el Triásico Tardío al Reciente. En el Sur de México y en el Sur occidente del Golfo de México se interpretaron las mega secuencias estratigráficas siguientes: (1) transgresión durante el Mesozoico; (2) regresión durante el Paleógeno; (3) regresión durante el Neógeno; (4) regresión y transgresión durante el PleistocenoHoloceno tardío y (5) estabilidad eustática actual a partir del Holoceno tardío, con base en la información geológica-geofísica del subsuelo marino y continental proporcionada por PEMEX-IMP, e integrada con aquella previamente establecida por diversos autores sobre las secuencias estratigráficas que afloran en la Sierra de Chiapas, y verificadas en localidades selectas durante este estudio, así como con los datos del Cuaternario aportados en este trabajo. En el área de estudio, se elaboró el mapa morfobatimétrico mediante un barrido continuo, utilizando las ecosondas hidro-acústicas del buque oceanográfico &#8220;Justo Sierra&#8221; de la UNAM, destacándose los sistemas de fallas más prominentes y las intrusiones salinas que afloran en el piso marino; la información geológica-marina de este estudio se complementó con los datos estratigráficos de pozos y con los perfiles sísmo-estratigráficos del subsuelo marino profundo, proporcionados por PEMEX-IMP. Con esta información integrada, se interpreta en este trabajo el movimiento dextrógiro del bloque de Yucatán que se desplaza en su porción Sur en Centro América, a lo largo de la provincia geológica del Arco de la Libertad y del sistema de fallas Polochic, con desplazamiento lateral-izquierdo. Los movimientos tectónicos dextrógiros de la microplaca de Yucatán fueron especialmente importantes durante el Mioceno tardío-Plioceno temprano, porque se reactivaron subsidentemente las cuencas Terciarias distensivas de Macuspana, Comalcalco y Salina del Istmo en el Sureste de México.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[Suroeste del Golfo de México]]></kwd>
<kwd lng="es"><![CDATA[tectónica]]></kwd>
<kwd lng="es"><![CDATA[sedimentación]]></kwd>
<kwd lng="es"><![CDATA[estratigrafía]]></kwd>
<kwd lng="en"><![CDATA[South western Gulf of Mexico]]></kwd>
<kwd lng="en"><![CDATA[tectonics]]></kwd>
<kwd lng="en"><![CDATA[sedimentation]]></kwd>
<kwd lng="en"><![CDATA[stratigraphy]]></kwd>
</kwd-group>
</article-meta>
</front><back>
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