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• W2073553752 abstract "Abstract To trace the sources and pathways of Zn in hydrothermal systems, the Zn isotope compositions of seventeen water samples from eight thermal springs and six gas samples from two fumaroles from La Soufriere, an active volcano on Guadeloupe Island (French West Indies, FWI), were analyzed using a method adapted for purifying Zn from Fe- and SO4-enriched thermal solutions. The fumaroles are enriched in Zn 100 to 8000 times compared to the local bedrock and have isotopic compositions (δ66Zn values from +0.21‰ to +0.35‰) similar to or slightly higher than fresh andesite (+0.21‰). The enrichment of Zn in the thermal springs compared with the surface waters shows that Zn behaves as a soluble element during hydrothermal alteration but is significantly less mobile than Na. The δ66Zn values of most of the spring waters are relatively constant (approximately 0.70‰), indicating that the thermal springs from La Soufriere are enriched in heavy isotopes (i.e., 66Zn) compared to the host rocks (from −0.14‰ to +0.42‰). Only three thermal springs have lower δ66Zn values (as low as −0.43%). While the Zn in the fumaroles is essentially derived from magma degassing, which is consistent with a previous study on Merapi volcano ( Toutain et al., 2008 ), we show that the Zn in the thermal springs is mainly derived from water–rock interactions. The 66Zn-enriched isotopic signature in most of the spring waters can be explained qualitatively by the precipitation at depth of sulfide minerals that preferentially incorporate the light isotopes. This agrees with the isotopic fractionation that was recently calculated for aqueous complexes of Zn. The few thermal springs with lower δ66Zn values also have low Zn concentrations, indicating the preferential scavenging of heavy Zn isotopes in the hydrothermal conduits. This study shows that unlike chemical weathering under surface conditions, hydrothermal alteration at high temperatures significantly fractionates Zn isotopes and enriches thermal waters in heavy Zn isotopes (e.g., 66Zn). Continental hydrothermal systems therefore constitute a source of heavy Zn isotopes to the oceans; this should be taken into account in the global oceanic budget of Zn." @default.
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• W2073553752 date "2014-02-01" @default.
• W2073553752 modified "2023-09-24" @default.
• W2073553752 title "Zn isotope compositions of the thermal spring waters of La Soufrière volcano, Guadeloupe Island" @default.
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• W2073553752 cites W1649947189 @default.
• W2073553752 cites W1966983664 @default.
• W2073553752 cites W1968175026 @default.
• W2073553752 cites W1969230161 @default.
• W2073553752 cites W1974104578 @default.
• W2073553752 cites W1974945390 @default.
• W2073553752 cites W1976598272 @default.
• W2073553752 cites W1977229510 @default.
• W2073553752 cites W1977970105 @default.
• W2073553752 cites W1980549980 @default.
• W2073553752 cites W1987619021 @default.
• W2073553752 cites W1992525388 @default.
• W2073553752 cites W1992743158 @default.
• W2073553752 cites W1992794581 @default.
• W2073553752 cites W1996901074 @default.
• W2073553752 cites W1997804883 @default.
• W2073553752 cites W2000169514 @default.
• W2073553752 cites W2000556874 @default.
• W2073553752 cites W2004272127 @default.
• W2073553752 cites W2007256017 @default.
• W2073553752 cites W2008294655 @default.
• W2073553752 cites W2009009356 @default.
• W2073553752 cites W2012873089 @default.
• W2073553752 cites W2014333124 @default.
• W2073553752 cites W2018648623 @default.
• W2073553752 cites W2019180529 @default.
• W2073553752 cites W2019315183 @default.
• W2073553752 cites W2020389567 @default.
• W2073553752 cites W2021134687 @default.
• W2073553752 cites W2021498615 @default.
• W2073553752 cites W2034803438 @default.
• W2073553752 cites W2036962611 @default.
• W2073553752 cites W2037076513 @default.
• W2073553752 cites W2037553433 @default.
• W2073553752 cites W2042764258 @default.
• W2073553752 cites W2044044672 @default.
• W2073553752 cites W2047410226 @default.
• W2073553752 cites W2058088400 @default.
• W2073553752 cites W2059623131 @default.
• W2073553752 cites W2062197462 @default.
• W2073553752 cites W2062496409 @default.
• W2073553752 cites W2063263639 @default.
• W2073553752 cites W2065295807 @default.
• W2073553752 cites W2067992793 @default.
• W2073553752 cites W2070358494 @default.
• W2073553752 cites W2077790399 @default.
• W2073553752 cites W2078060103 @default.
• W2073553752 cites W2079845362 @default.
• W2073553752 cites W2080343071 @default.
• W2073553752 cites W2081264066 @default.
• W2073553752 cites W2084343178 @default.
• W2073553752 cites W2084817317 @default.
• W2073553752 cites W2088516268 @default.
• W2073553752 cites W2093696105 @default.
• W2073553752 cites W2094352778 @default.
• W2073553752 cites W2102484660 @default.
• W2073553752 cites W2109022677 @default.
• W2073553752 cites W2110688948 @default.
• W2073553752 cites W2114134135 @default.
• W2073553752 cites W2114377783 @default.
• W2073553752 cites W2117807252 @default.
• W2073553752 cites W2120777708 @default.
• W2073553752 cites W2123232386 @default.
• W2073553752 cites W2128840954 @default.
• W2073553752 cites W2140784809 @default.
• W2073553752 cites W2145385939 @default.
• W2073553752 cites W2147124700 @default.
• W2073553752 cites W2152743530 @default.
• W2073553752 cites W2158749397 @default.
• W2073553752 cites W2160113469 @default.
• W2073553752 cites W2170503874 @default.
• W2073553752 doi "https://doi.org/10.1016/j.gca.2013.11.022" @default.
• W2073553752 hasPublicationYear "2014" @default.
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