Near shore submarine hydrothermal activity in Bahia Banderas, western Mexico

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Autore principale: Rosa María Prol Ledesma
Natura: Artículo científico
Lingua:en
Pubblicazione: Universidad Nacional Autónoma de México 2000
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author Rosa María Prol Ledesma
author_facet Rosa María Prol Ledesma
contents Near shore submarine hydrothermal activity in Bahia Banderas, western Mexico Rosa María Prol Ledesma F. J. Núñez Cornú A. Cupul Magaña C. Suárez Plascencia Ciencias de la Tierra Mexico sulfide deposition underwater hydrothermal vents Shallow submarine hydrothermal activity was detected in the Bahía de Banderas area, Mexico. Volcanic-type tremors wererecorded by portable seismological stations onshore. Vent samples suggest a depositional sequence dominated by carbonates inthe first stage (calcite and dolomite), followed by apatite and late barite veins. Layers of sequential deposition of sulfides were alsoobserved, and are interpreted as cyclic variations of sulphur fugacity. 2000 artículo científico 0016-7169 https://www.redalyc.org/articulo.oa?id=56839203 en http://www.redalyc.org/revista.oa?id=568 Geofísica Internacional application/pdf Universidad Nacional Autónoma de México Geofísica Internacional (México) Num.2 Vol.39
format Artículo científico
id redalyc_56839203
institution Redalyc
language en
publishDate 2000
publisher Universidad Nacional Autónoma de México
spellingShingle Near shore submarine hydrothermal activity in Bahia Banderas, western Mexico
Rosa María Prol Ledesma
Ciencias de la Tierra
Mexico
sulfide deposition
underwater hydrothermal vents
Near shore submarine hydrothermal activity in Bahia Banderas, western Mexico Rosa María Prol Ledesma F. J. Núñez Cornú A. Cupul Magaña C. Suárez Plascencia Ciencias de la Tierra Mexico sulfide deposition underwater hydrothermal vents Shallow submarine hydrothermal activity was detected in the Bahía de Banderas area, Mexico. Volcanic-type tremors wererecorded by portable seismological stations onshore. Vent samples suggest a depositional sequence dominated by carbonates inthe first stage (calcite and dolomite), followed by apatite and late barite veins. Layers of sequential deposition of sulfides were alsoobserved, and are interpreted as cyclic variations of sulphur fugacity. 2000 artículo científico 0016-7169 https://www.redalyc.org/articulo.oa?id=56839203 en http://www.redalyc.org/revista.oa?id=568 Geofísica Internacional application/pdf Universidad Nacional Autónoma de México Geofísica Internacional (México) Num.2 Vol.39
title Near shore submarine hydrothermal activity in Bahia Banderas, western Mexico
topic Ciencias de la Tierra
Mexico
sulfide deposition
underwater hydrothermal vents
url https://www.redalyc.org/articulo.oa?id=56839203