Please use this identifier to cite or link to this item: http://nopr.niscpr.res.in/handle/123456789/1881
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dc.contributor.authorChudaev, O.-
dc.contributor.authorChudaeva, V.-
dc.contributor.authorSugimori, K.-
dc.contributor.authorKuno, A.-
dc.contributor.authorMatsuo, M.-
dc.date.accessioned2008-08-25T10:24:37Z-
dc.date.available2008-08-25T10:24:37Z-
dc.date.issued2008-06-
dc.identifier.issn0379-5136-
dc.identifier.urihttp://hdl.handle.net/123456789/1881-
dc.description166-180en_US
dc.description.abstractThe resent study consists the original geochemical data on the thermal waters of the Kuril Islands (Mendeleev, Golovnin, and Ebeko volcanoes) and relation between thermal waters and ore formation. Among the thermal water types three main groups can be distinguished: sodium–chloride, acid sulfate and chloride-sulfate-bicarbonate. The contents and behaviors of siderophile, chalcophile, lithophile, and rare-earth elements are discussed. These data, together with the result of isotopic studies, enumerates the origin of these waters. The high-temperature sodium-chloride waters have a profound effect on the formation of copper-pyrite mineralization on Mendeleev, Ebeko and Baransky volcanoes. The acid waters influence the processes of hypergenic ore formationen_US
dc.language.isoen_USen_US
dc.publisherCSIRen_US
dc.sourceIJMS Vol.37(2) [June 2008]en_US
dc.subjectGeochemistry of thermal watersen_US
dc.subjectStable isotopesen_US
dc.subjectOre formationen_US
dc.subjectKuril Islandsen_US
dc.titleComposition and origin of modern hydrothermal systems of the Kuril island arcen_US
dc.typeArticleen_US
Appears in Collections:IJMS Vol.37(2) [June 2008]

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