Near shore submarine hydrothermal activity in Bahia Banderas, western Mexico

dc.contributorNúñez-Cornú, F.J., CUC, Universidad de Guadalajara, Puerto Vallarta, Jal., Mexico, SIS VOC, CUC, Universidad de Guadalajara, Av. Universidad 203, Puerto Vallarta, Jal., Mexico; Prol-Ledesma, R.M., Instituto de Geofísica, UNAM, Cd. Universitaria, 04510 México, D.F., Mexico; Cupul-Magaña, A., CUC, Universidad de Guadalajara, Puerto Vallarta, Jal., Mexico, SIS VOC, CUC, Universidad de Guadalajara, Av. Universidad 203, Puerto Vallarta, Jal., Mexico; Suárez-Plascencia, C., CUC, Universidad de Guadalajara, Puerto Vallarta, Jal., Mexico, SIS VOC, CUC, Universidad de Guadalajara, Av. Universidad 203, Puerto Vallarta, Jal., Mexico
dc.creatorNunez-Cornu, F.J.
dc.creatorProl-Ledesma, R.M.
dc.creatorCupul-Magana, A.
dc.creatorSuarez-Plascencia, C.
dc.date.accessioned2015-11-19T18:51:17Z
dc.date.accessioned2022-11-02T14:39:06Z
dc.date.available2015-11-19T18:51:17Z
dc.date.available2022-11-02T14:39:06Z
dc.date.created2015-11-19T18:51:17Z
dc.date.issued2000
dc.identifierhttp://hdl.handle.net/20.500.12104/66409
dc.identifierhttp://www.scopus.com/inward/record.url?eid=2-s2.0-0033882707&partnerID=40&md5=9226a6c9afda6ba62bce109909be3c99
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/5001842
dc.description.abstractShallow submarine hydrothermal activity was detected in the Bahia de Banderas area, Mexico. Volcanic-type tremors were recorded by portable seismological stations onshore. Vent samples suggest a depositional sequence dominated by carbonates in the first stage (calcite and dolomite), followed by apatite and late barite veins. Layers of sequential deposition of sulfides were also observed, and are interpreted as cyclic variations of sulphur fugacity.
dc.relationGeofisica Internacional
dc.relation39
dc.relation2
dc.relation171
dc.relation178
dc.relationScopus
dc.titleNear shore submarine hydrothermal activity in Bahia Banderas, western Mexico
dc.typeArticle


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