Циркон-Пойнт

Циркон-Пойнт пегматит, Хмара-Бэй, Напир комплекс, Земля Эндерби, Антарктида \ Zircon point pegmatite, Khmara Bay, Casey Bay, Napier Complex, Enderby Land, Eastern Antarctica, Antarctica; 67°20'S , 49°0'E \\ Источник: http://www.mindat.org/loc-125924.html

Минералы

магнезиотааффеит-6N'3S \ magnesiotaaffeite-6N'3S; суринамит ; *хмаралит--http://www.mindat.org/min-7136.html; хризоберилл \\

Литература

Barbier, J., Grew, E.S., Moore, P.B., and Su, S.-C. (1999) Khmaralite, a new beryllium-bearing mineral related to sapphirine: A superstructure resulting from partial ordering of Be, Al and Si on tetrahedral sites. American Mineralogist: 84: 1650-1660.
Grew E.S. Surinamite, taafeite and beryllian saphirine from pegmatites in graulite-facies rocks of Casey Bay , Enderby Land, Antarctica , - Am. Miner., 1981,v.66, p.1022-1033.
Grew E.S., Yates M.G., Barbier J., Shearer C.K., Sheraton J.W., Shiraishi K., et al. (2000,October). Granulite-facies beryllium pegmatites in the Napier Complex in Khmara and Amundsen bays, western Enderby Land, East Antarctica . - Polar Geoscience, 13, 1-40
Kristiansen, R.(2000): Eksotiske mineral-lokaliteter (Exotic mineral-locations). STEIN 27 (2), 20-24