Abstract
SERICITE, otherwise known as hydromuscovite, is a product of hydrothermal alteration of granodiorite and occurs as aggregates of fine grains with a silky lustre. It has the chemical composition shown in Table 1 (1).
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References
Brindley, G. W., Amer. Mineralogist, 41, 91 (1956).
Brown, G., and Weir, A. H., Intern. Clay Conf., 1963 (CIPEA, Pergamon Press, 1963).
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UEDA, S., SUDO, T. Synthesis of an Interstratified Mineral from Micas. Nature 211, 1393–1394 (1966). https://doi.org/10.1038/2111393a0
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DOI: https://doi.org/10.1038/2111393a0
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