The occurrence of giant andalusite crystals in the pegmatites of Szabo Bluff reflects the position of the aluminosilicate triple point relative to the granite minimum melting curve and indicates an extremely restricted set of crystallization conditions at relatively low P and moderate T.-G.R.M.
|Original language||English (US)|
|Number of pages||4|
|Journal||Antarctic Journal of the United States|
|State||Published - Jan 1 1983|
ASJC Scopus subject areas
- Earth and Planetary Sciences(all)