Fluid evolution of rare-element and muscovite granitic pegmatites from central Galicia, NW Spain

Fluid inclusions have been studied in three pegmatite fields in Galicia, NW Iberian Peninsula. Based on microthermometry and Raman spectroscopy, eight fluid systems have been recognized. The first fluid may be considered to b e a pegmatitic fluid which is represented by daughter mineral (silicates)-r ich aqueous inclusions. These inclusions are primary and formed above 500 d egrees C (dissolution of daughter minerals). During pegmatite crystallizati on, this fluid evolved to a low-density, volatile-rich aqueous fluid with l ow salinity (93% H2O; 5% CO2; 0.5% CH4; 0.2% N-2; 1.3% NaCl) at minimum P-T conditions around 3 +/- 0.5 kbar and 420 degrees C. This fluid is related to rare-metal mineralization. The volatile enrichment may be due to mixing of magmatic fluids and fluids equilibrated with the host rock. A drop in pr essure from 3 +/- 0.5 to 1 kbar at a temperature above 420 degrees C, which may be due to the transition from predominantly lithostatic to hydrostatic pressure, is recorded by two-phase, water-rich inclusions with a low-densi ty vapour phase (CO2, CH4 and N-2) Another inclusion type is represented by two-phase, vapour-rich inclusions with a low-density vapour phase (CO2, CH 4 and N-2), indicating a last stage of decreasing temperature (360 degrees C) and pressure (around 0.5 kbar), probably due to progressive exhumation. Finally, volatile (CO2)-rich aqueous inclusions, aqueous inclusions (H2O-Na Cl) and mixed-salt aqueous inclusions with low Th, are secondary in charact er and represent independent episodes of hydrothermal fluid circulation bel ow 310 degrees C and 0.5 kbar.