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The classic model of hydrothermal alteration of the upper oceanic crust identifies epidosites (basalts altered to epidote + quartz + titanite ± Fe-oxides) as markers of discharging hydrothermal fluid. Epidosites are depleted in metals and therefore
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https://explore.openaire.eu/search/publication?articleId=doi_________::44ada9e14ccaae3b3230e4093bd0407e
