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Accessory minerals from the Primorsky rapakivi granite complex, West Baikal Region

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Abstract

The composition of accessory minerals from granites of the second phase, quartz-muscovite (+fluorite), and quartz-muscovite-topaz greisens from the Primorsky rapakivi granite complex, West Baikal region, were studied using backscattered scanning electron microscopy. Ilmenite from granites contains inclusions of cassiterite, titanocolumbite, fergusonite-(Y), polycrase-(Y), and betafite. Allanite-(Ce), bastnaesite-(Ce), xenotime-(Y), Y- and Zr-thorite, zircon, and cyrtolite have been identified in granites. Greisens contain cassiterite, ferrocolumbite (Ta/Nb = 0.02−0.06), pyrochlore-group minerals, ilmenorutile, rutile, wolframite, polycrase-(Y), monazite-(Ce), fluocerite-(Ce), bastnaesite-(Ce), cerphosphorhuttonite, thorite, and other minerals. The ferrocolumbite + ilmenorutile assemblage is typical of quartz-muscovite greisen, whereas the rutile + ilmenorutile + wolframite + W-columbite assemblage is contained in the quartzmuscovite-topaz greisen as a result of an increase in Eh and decrease in pH and potassium activity of solution in the back zone. The compositions of Th- and REE-bearing minerals indicate the important role of phosphate and fluorine complexes in the transport of these elements.

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Correspondence to V. B. Savel’eva.

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Original Russian Text © V.B. Savel’eva, E.P. Bazarova, N.S. Karmanov, 2011, published in Zapiski RMO (Proceedings of the Russian Mineralogical Society), 2011, No. 2, pp. 38–58.

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Savel’eva, V.B., Bazarova, E.P. & Karmanov, N.S. Accessory minerals from the Primorsky rapakivi granite complex, West Baikal Region. Geol. Ore Deposits 53, 708–722 (2011). https://doi.org/10.1134/S1075701511080149

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