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- W2044438530 abstract "The Middle Proterozoic granitic massif, in the Goiás Tin Province, is affected by pervasive post-magmatic hydrothermal alterations, chiefly by eastward, increasingly developed greisenization. Hydrothermal alteration results in strong mineralogical and chemical modifications of granite composition, but nevertheless the effect of fluid circulations is probably limited to a dilution of the initial REE content in magmatic rocks without any important fractionation, as suggested by the similarity between chondrite-normalized patterns for all rocks, from the less altered granite to the muscovite-topaz-bearing greisen. Le massif granitique du Protérozoïque moyen de Serra Branca, dans la province stannifère de Goiás, est affecté dans son ensemble par des altérations hydrothermales post-magmatiques, dont la principale est une greisénisation, d'intensité croissante d'ouest en est. L'altération hydrothermale a fortement modifié la minéralogie et le chimisme des granités, mais, cependant, les circulations de fluides ont probablement entraîné une simple dilution du stock initial de terres rares dans les roches magmatiques, sans fractionnement important, comme le suggère la similitude des spectres normalisés dans toutes les roches, depuis le granité le moins transformé jusqu'au greisen à muscovite et topaze." @default.
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- W2044438530 date "1999-05-01" @default.
- W2044438530 modified "2023-09-27" @default.
- W2044438530 title "Mobilité des terres rares au cours des altérations hydrothermales: l'exemple du granité de Serra Branca, Brésil central" @default.
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- W2044438530 doi "https://doi.org/10.1016/s1251-8050(99)80175-x" @default.
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