A B S TR A CT Some granulites from the Amessmessa area (south In Ouzzal unit, Hoggar) contain the peak assemblage gedrite+garnet+sillimanite+quartz that was used to estimate the P-T conditions of metamorphism. The rocks developed symplectites and corona textures by the breakdown of the primary paragenesis to orthopyroxene, cordierite and spinel. The successive parageneses formed in separate microdomains according to a clockwise P-T path. Geothermometry, geobarometry and phase diagram calculations indicate that the textures formed by decompression and cooling from 7-9 kbar and 850-900°C to 3.5-4.5 kbar and 700-800°C. This P-T evolution is consistent with low to medium a H2O, between 0.4 and 0.7, and is similar to the metamorphic conditions deduced in Al-Mg granulites from the north of In Ouzzal.

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