Abstract
Electron probe microanalyses of 38 muscovites from Warramunga rocks, “porphyroidal” rocks and from magnetite rocks of lode structures of Tennant Creek field were carried out. Recrystallisation of muscovite, progressive in Warramunga rocks and retrogressive in “porphyroidal” rocks was contemporaneous and took place under lower green schist facies conditions of metamorphism during regional deformation. Muscovite in the magnetite lode structures and the country rock had formed ahead of the sulphide mineralisation on the Warramunga rocks subsequent to their regional metamorphism and was due to metasomatic alteration on the wall rocks.
The analysed muscovites conform to phengite mica but some of them have Si in excess of the stipulated limit of 3·5 units per half unit cell. The analysed phengites show a shift in the layer charge from tetrahedral to octahedral layer conforming to trisilicictetrasilicic series. The (Si +R 2+) and (AlVI + AlIV) show positive correlation. The author advocates that the term phengite be retained to describe all the intermediate members of the potassium dioctahedral micas including those having Si in excess on the stipulated limit.
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Rao, T.R. Electron probe microanalyses of muscovites from low grade metamorphic rocks of Tennant Creek area, Central Australia. Proc. Indian Acad. Sci. 83, 150–159 (1976). https://doi.org/10.1007/BF03045704
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DOI: https://doi.org/10.1007/BF03045704