<?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>S1405-33222006000100083</article-id>
<article-id pub-id-type="doi">10.18268/bsgm2006v58n1a3</article-id>
<title-group>
<article-title xml:lang="es"><![CDATA[Procesos de mineralización en manantiales hidrotermales submarinos someros. Ejemplos en México]]></article-title>
<article-title xml:lang="en"><![CDATA[Mineralizing processes at shallow submarine hydrothermal vents: examples from Mexico]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Canet]]></surname>
<given-names><![CDATA[Carles]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Prol-Ledesma]]></surname>
<given-names><![CDATA[Rosa María]]></given-names>
</name>
<xref ref-type="aff" rid="Aff"/>
</contrib>
</contrib-group>
<aff id="Af1">
<institution><![CDATA[,Universidad Nacional Autónoma de México Instituto de Geofísica ]]></institution>
<addr-line><![CDATA[México ]]></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>83</fpage>
<lpage>102</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S1405-33222006000100083&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S1405-33222006000100083&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S1405-33222006000100083&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[Resumen El estudio geoquímico y mineralógico realizado en varias localidades con manantiales hidrotermales submarinos someros (emplazados a menos de 200 mbnm) sugiere que este tipo de actividad puede haber generado yacimientos importantes de óxidos, sulfuros y metales preciosos. La relevancia del estudio de estos sistemas de manantiales reside en el hecho de que, además de ser los análogos actuales de algunos depósitos metalíferos de interés económico, éstos soportan ecosistemas especializados, caracterizados por la coexistencia y competencia de organismos quimiosintéticos y fotosintéticos. En relación a la actividad metabólica de los primeros tienen lugar algunos procesos biogeoquímicos y de mineralización similares a los que se han descrito en ambientes oceánicos de chimeneas mineralizantes y en infiltraciones frías de hidrocarburos. La profundidad máxima que define a los manantiales hidrotermales submarinos someros como tales es de 200 m. Este límite de profundidad determina un cambio brusco en los parámetros ambientales y de estructura de las comunidades bióticas, y coincide con un aumento en la pendiente de la curva de ebullición respecto a la presión para el agua marina. Los fluidos hidrotermales de los manantiales submarinos someros presentan características químicas e isotópicas intermedias entre los de los manantiales de gran profundidad y los de los sistemas geotérmicos continentales. Generalmente, la salinidad del agua termal es inferior a la del agua de mar, lo cual implica, junto con la composición isotópica, la presencia en el fluido de una importante componente de agua meteórica. Un rasgo característico de los sistemas hidrotermales someros es la presencia de una fase gaseosa exsuelta, que en muchos casos es muy rica en CO2. Dicha fase puede contener, además, cantidades elevadas de N2 y CH4 en sistemas cuyos fluidos interaccionan con sedimentos, y de H2S en sistemas vinculados a actividad fumarólica de volcanes. En las costas occidentales de México se conocen sistemas hidrotermales submarinos someros en Punta Banda y Bahía Concepción en la península de Baja California, y en Punta Mita en Nayarit. Dichos sistemas están emplazados en contextos de margen continental afectado por extensión tectónica con un elevado gradiente geotérmico, y en ningún caso presentan vínculos claros con actividad volcánica. Su estudio ha generado un volumen importante de información acerca de sus características geoquímicas y mineralógicas, así como de los procesos que desencadenan la precipitación de minerales alrededor de las zonas de descarga de fluidos hidrotermales. Además, los sistemas de manantiales hidrotermales someros podrían suponer una potencial fuente de energía geotérmica.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[Abstract Recent mineralogical and geochemical studies on shallow submarine hydrothermal vents (at water depths &lt; 200 mbsl) suggest that their activity could have been responsible for the formation of oxide, sulfide and precious metal-bearing ores. Therefore, shallow submarine vents may be considered as modern analogues of some economic ore deposits. The boundary between shallow and deep hydrothermal vents can be established at a depth of 200 mbsl, which represents an abrupt change in the environmental parameters and in the structure of the biotic communities. In addition, this depth corresponds to an increase of the slope of the boiling curve of seawater with respect to pressure. Shallow submarine vents support complex specialized biotic communities, characterized by the coexistence and competition of chemosynthetic and photosynthetic organisms. Some biogeochemical and biomineralization processes related to chemosynthesis are similar to those described in deep ocean hydrothermal vents and in cold seeps. Hydrothermal shallow vent fluids show intermediate chemical and isotopic characteristics between those of deep vents and of continental geothermal systems. Commonly, vent water has lower salinities than seawater. This fact, along with isotopic compositions, is evidence for large contributions of meteoric water in these vents. Venting of exsolved gas, evidenced by continuous bubbling, is a striking feature of shallow submarine hydrothermal systems. In most cases vent gas is rich in CO2, but it can be rich in N2 and CH4 in vent systems related to thick sedimentary series, and rich in H2S in vents related to volcanic fumaroles. In Mexico, shallow submarine hydrothermal venting has been reported in Punta Banda and Bahía Concepción in Baja California Peninsula, and in Punta Mita in Nayarit. The tectonic setting of these hydrothermal systems corresponds to continental margins affected by extension, with anomalously high geothermal gradients. These vents do not show obvious links with volcanic activity. Their study has contributed to the understanding of mineralogical and geochemical processes in shallow submarine hydrothermal vents. These systems, in addition, may be a potential source of geothermal energy.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[Manantiales hidrotermales]]></kwd>
<kwd lng="es"><![CDATA[zona nerítica]]></kwd>
<kwd lng="es"><![CDATA[quimiosíntesis]]></kwd>
<kwd lng="es"><![CDATA[yacimientos minerales]]></kwd>
<kwd lng="en"><![CDATA[Hydrothermal vents]]></kwd>
<kwd lng="en"><![CDATA[neritic zone]]></kwd>
<kwd lng="en"><![CDATA[chemosynthesis]]></kwd>
<kwd lng="en"><![CDATA[ore deposits]]></kwd>
</kwd-group>
</article-meta>
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