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Iron sulfides formation in modern estuaries: some genetic considerations

dc.contributor.authorBorrego Flores, José 
dc.contributor.authorMorales González, Juan Antonio 
dc.contributor.authorPendón Martín, José Gabriel 
dc.date.accessioned2020-05-18T09:25:48Z
dc.date.available2020-05-18T09:25:48Z
dc.date.issued1991
dc.identifier.urihttp://hdl.handle.net/10272/17986
dc.description.abstractIron sulfides found in estuaries located along the mesotidal coast of Huelva (SW Iberia) show various kinds of occurrence and allow to infer their genesis as an early diagenetic process. Sediment burial produces the alteration of organic matter and the reduction of ferric iron which reacts with amorfous iron grains supplied by Plio-Pleistocene sediments from the substrate. Sulfates supplied by marine waters can produce reduction of sulfur. Iron sulfides precipitation is then taken into accountes_ES
dc.language.isospaes_ES
dc.publisherSociedad Geológica de Españaes_ES
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherIron sulfideses_ES
dc.subject.otherEstuarieses_ES
dc.subject.otherEarly diagenesises_ES
dc.subject.otherHuelvaes_ES
dc.titleFormación de sulfuros de hierro en estuarios actuales: algunas consideraciones genéticases_ES
dc.titleIron sulfides formation in modern estuaries: some genetic considerationseng
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES


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