Ip. Solovova et al., INCLUSION COMPOSITION IN MINERALS AND CRY STALLIZATION CONDITIONS OF RARE-METAL BEARING GRANITES OF HOMRAT-AKAREM (EGYPT), Geohimia, (7), 1994, pp. 956-967
Melt, solid and fluid microinclusions in quartz of rare metal bearing
granited are studied. P-T Parameters of main stages in granitic magma
evolution containing fluorine (up to 0.5 mass % F), water (9-10 mass %
H2O). These stages are characterised by the following parameters: 1)
quartz crystallization at 640-degrees-C, and 8 kbar; 2) complete solid
ification of the melt at 500-550-degrees-C; and 4-5 kbar; 5) microschl
ieren aggregates in granites are crystallised at 300-degrees-C and 0.4
kbar. Magmatic origin of topaz and fluorite is evidenced.