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Volatile‐Rich Hydrothermal Plumes Over the Southern Central Indian Ridge, 24°49’S: Evidence for a New Hydrothermal Field Hosted by Ultramafic Rocks
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2022
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Source: Geochemistry, Geophysics, Geosystems, 23(10)
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Journal Title:Geochemistry, Geophysics, Geosystems
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Description:Water column physico-chemical studies were conducted over the southern Central Indian Ridge between 24°44’S and 25°52’S to identify and chemically characterize seafloor hydrothermal activity. High turbidity values were observed between 2300 and 2700 m with two distinct layers, between water depths of 2320–2500 m and 2510–2650 m, at two closely spaced CTD stations at 24°48.62’S (CTD-17-P5) and 24°48.68’S (CTD-17-P8). Elevated concentrations of dissolved Mn (DMn: 19–112 nM), dissolved Fe (DFe: 33–88 nM), methane (CH4: 32–246 nM), elevated δ 3He values (28%–88%), and stable carbon isotope ratios of CH4 confirm the hydrothermal origin. In plume layer-1, the maximum concentrations were observed at
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Source:Geochemistry, Geophysics, Geosystems, 23(10)
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DOI:
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ISSN:1525-2027;1525-2027;
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Rights Information:CC BY-NC-ND
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Compliance:Library
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