Fluid evolution and exhumation path of the Trivandrum Granulite Block, southern India

In charnockites and host garnet-biotite gneisses of the Trivandrum Granulite Block (TGB), southern India, fluid inclusions are mainly represented by CO 2-rich categories. Aqueous inclusions with low salt concentration (0.33-13.5 wt% NaCl equiv.) occur subordinately. We recognize three generations of CO 2-rich inclusions, which have contrasting fluid densities that correlate with the different stages of metamorphic evolution established from mineral phase equilibria studies . Although some of these inclusions show variable depression in melting temperatures, laser Raman spectroscopic studies revealed no volatiles other than CO 2. We report here the occurrence of high-density CO 2-rich inclusions for the first time from this region with homogenization temperatures in the range of -21.9 to-15.6 degrees C (?=1.041-1.012 g/cm 3). The marked secondary character of these high-density inclusions and their textural association with late brittle deformational features indicate their entrapment at low temperature conditions (250-300 degrees C), post-dating charnockite formation. Regional metamorphism in TGB (stage M1) took place at ca. 700 degrees C and 5.36 kbar, although higher temperatures prevailed in the northern part of the terrain. A subsequent period of decompression (of the order of 6-7 km) was accompanied by partial recrystallization of host rocks and intensive processes of charnockite formation (M2) that extended to subisobaric cooling from 785-805 to 680-700 degrees C. The relatively small population of aqueous inclusions in charnockites and their low salinity preclude any major role for metasomatic processes involving increase of potassium activity, and confirm the important role of CO 2-rich fluids in stabilizing low water activities. During the final phase of exhumation of the region (ca. 9 km in depth), additional heat input resulted in mineralogical alterations correlated to stage M3. While the source of heat and fluids involved in charnockite formation is postulated to be magmas derived from sublithospheric sources, the late heat and fluid transfer are correlated to late Pan-African ultrabasic and alkaline intrusives emplaced at shallow depths.