Abstract
The P-T conditions of formation of granulites from Salvador, Bahia, were determined by some available geothermometers and geobarometers. At least, three phases of polimetamorphism were recognized: 7,5 kbar and 840-900 o C; 6,75-7,5 kbar and 525-550°C; and around 3 kbar 750°C.
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