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The biogenic influence in the formation of massive sulphide deposits of the Iberian Pyrite Belt

dc.contributor.authorTornos, Fernando
dc.contributor.authorConde, C.
dc.date.accessioned2014-11-18T12:18:44Z
dc.date.available2014-11-18T12:18:44Z
dc.date.issued2002
dc.identifier.urihttp://hdl.handle.net/10272/9335
dc.description.abstractThe Tharsis supergiant massive sulphide deposits shows evidence of being formed by exhalative processes on the seafloor. The carbonate-siderite ore is interpreted as a bacterial mound while the bulk of the orebody seems to be formed in a brine pool by mixing of sulphur-depleted deep brines with H2S generated by hyperthermophile (archeo-)bacteria in the chemoclyne. This mechanism is significantly slower but geochemically much more effective that mound accretion on the seafloor and is interpreted as being the reason of the presence of supergiant massive sulphide deposits in the Iberian Pyrite Belten_US
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherMassive sulphidesen_US
dc.subject.otherIberian Pyrite Belten_US
dc.subject.otherTermophile bacteriaen_US
dc.titleLa influencia biogénica en la formación de los yacimientos de sulfuros masivos de la Faja Pirítica Ibéricaen_US
dc.titleThe biogenic influence in the formation of massive sulphide deposits of the Iberian Pyrite Belteng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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