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- W2290909963 abstract "Large lenses of sillimanite occur in biotite-sillimanite schist 60 to 70 km west of Pofadder, South Africa, in the Wortel Formation of the Bushmanland Group. In one of the abandoned sillimanite quarries on the farms Hotson and Koenabib, the paragenesis sillimanite - natroalunite - zaherite - hotsonite was found. It is associated with silicates (kaolinite, pyrophyllite, topaz, muscovite and biotite), oxides (diaspore, rutile, ilmenite and corundum), sulfides (chalcopyrite, covellite and pyrite) and sulfide alteration products (covellite and goethite, atacamite and chalcanthite). The prevalent sequence of alteration is from sillimanite to natroalunite to zaherite to hotsonite, which is also the sequence of decreasing relative abundance, but sil limanite was directly transformed to zaherite wherever alkali elements were locally scanty. The necessary sulfate was apparently supplied during the oxidation of sulfides such as chalcopyrile and pyrite." @default.
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- W2290909963 date "1985-02-01" @default.
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- W2290909963 title "A natroalunite-zaherite-hotsonite paragenesis from Pofadder, Bushmanland, South Africa" @default.
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