1. Anfilogov, V.N., Abramov, V.A., Kovalenko, V.I., and Ogorodova, V.Ya., Phase relations in the agpaitic field of the Na2O-K2O-Al2O3-SiO2-H2O system at a pressure of 1000 kg/cm2, Dokl. Akad. Nauk SSSR, 1972, vol. 294, no. 4, pp. 944–947.
2. Bailey, D.K. and Macdonald, R., Alkali-feldspar fractionation trends and the derivation of peralkaline liquids, Am. J. Sci., 1969, vol. 267, no. 2, pp. 242–248.
3. Bakumenko, I.T. and Konovalenko, S.I., Specific features of the formation of miarolitic pegmatites and their position among granite pegmatites, in Termobarogeokhimicheskie issledovaniya protsessov mineraloobrazovaniya (Studies of Inclusions in Minerals with Applications to Mineral Formation), Sobolev, N.V. and Bakumenko, I.T., Eds., Novosibirsk: Nauka, 1988, pp. 123–135.
4. Balitsky, V.S., Kurashige, M., Balitskaya, L.V., and Iwasaki, W., Study of quartz solubility and “heavy” phase formation under industrial synthetic quartz growth conditions, Joint ISHR&ICSTR, Kochi: Kochi University, 2000, pp. 318–321.
5. Butuzov, V.P. and Bryatov, L.V., Study of phase equilibria in part of the H2O-SiO2-Na2CO3 system at high temperaures and pressures, Kristallografiya, 1957, vol. 204, no. 4, pp. 944–947.