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- W2358595883 abstract "We report on the composition of chlorite in altered rocks from active and fossil gmthermal systems, and from Neogene hydrothermal Cu-Pb-Zn vein-type and Kuroko deposits of Japan. Values of Fd+ /(F&+ + Mg) in chlorite from the ore deposits are more variable than in chlorite from the altered rocks of the geothermal systems. The, value Fd+/Mg of chlorite from the latter is positively correlated with that of the fresh rock, and thus seems controlled by the composition of the original rock. The variability in F&+ /Mg of chlorite from the Kuroko and Neogene vein-type deposits is attributed to a control by the fluid phase (Fea+/Mg, pH, ES, temperature). The influence of movement and mixing of fluid phases may also be important." @default.
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- W2358595883 date "1987-09-01" @default.
- W2358595883 modified "2023-09-25" @default.
- W2358595883 title "Compositional differences in chlorite from hydrothermally altered rocks and hydrothermal ore deposits" @default.
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