Geochemistry of muscovite from pegmatites of the Eastern Brazilian pegmatite province : a clue to petrogenesis and mineralization potential.
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2007
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Abstract
Single crystals of muscovite (N = 143) from different zones of selected granitic pegmatites belonging to two wellknown
gem-producing districts of the Eastern Brazilian Pegmatite Province (northern Araçuai and western Governador Valadares
in Minas Gerais) were analyzed for major, minor and trace elements. Structural formulae display considerable (Fe+Mg) variation
within the octahedral site, coupled with tetrahedral Si-Al substitution (Tschermak substitution – phengite component). Tetrahedral
Si varies from 3.06 to 3.21 and AlVI from 1.71 to 1.90 apfu.
Trace elements in muscovite are significant indicators for the economic potential of pegmatites as well as for the differentiation
degree and origin of the magma. Muscovite with higher Li and B contents is characteristic for gem-tourmaline-bearing pegmatites.
Lower concentrations in K/Rb, Ti and Mg and higher F contents are found in muscovites from higher differentiated zones within
the pegmatite. In comparison with anatectic pegmatites, relatively low K/Rb ratios of muscovite from the studied pegmatites are
indicative of derivation by fractional crystallization of granite magma. Zn, Ga and Y, elements rarely analyzed in micas, tend to
increase with decreasing K/Rb ratios, showing them to be good indicators of the fractionation degree of magmas.
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Keywords
Muscovite, Crystal chemistry, Trace elements
Citation
VIANA, R. R.; EVANGELISTA, H. J.; STERN, W. B. Geochemistry of muscovite from pegmatites of the Eastern Brazilian pegmatite province: a clue to petrogenesis and mineralization potential. European Journal of Mineralogy, v. 19, p. 745-755, 2007. Disponível em: <https://www.schweizerbart.de/papers/ejm/detail/19/57893/Geochemistry_of_muscovite_from_pegmatites_of_the_Eastern_Brazilian_pegmatite_province_a_clue_to_petrogenesis_and_mineralization_potential>. Acesso em: 20 de jun. 2017.