(Přibyslavice)
Small complex of Přibyslavice granite primarily consists of alkali-feldspar tourmaline-muscovite granite that chemically belongs to peraluminous (at places even hyperaluminous) granites. It is enriched by B, C, Cs, F, Li, Nb, P, Rb, Sn, Ta, U and Zn. Formation of Přibyslavice granite is considered to be a product of diffusion granitization of the metamorphosed substrate by an alkali-rich melt and subsequent younger albitization. Complex mineralization is divided into rock forming minerals (including almandine garnet) and accessories (sulfides, dumortierite etc.), pods and nests of primary and secondary Li-Fe-Mn-Ca-Zn phosphates, minerals of tin-bearing granite (cassiterite, nigerite), pegatite minerals (lepidolite etc.).
Ref.: Povondra, P., Pivec, E. (eds.) et al.: Přibyslavice peraluminuous granite. Acta universitatis carolinae, Geologica, 1987, no. 3, s . 183 – 283.
