DEHYDRATION-MELTING PHENOMENA IN LEPTYNITIC GNEISSES AND THE GENERATION OF LEUKOGRANITES - A CASE-STUDY FROM THE KERALA KHONDALITE BELT, SOUTHERN INDIA

Pan-African high-grade metamorphism in the Kerala Khondalite Belt (Sou th India) led to the in situ formation af garnet-bearing leucosomes (L 1) in sodic quartz-alkali feldspar-biotite gneisses. Microtextures, mi neralogy and the geochemical characteristics of in situ leucosomes (L1 ) and gneiss domains (GnD) indicate that the development of leucosomes was mainly controlled by the growth of garnet at the expense of bioti te. This is documented by the selective transfer of FeO, MgO, Upsilon, Sm and the heavy rare earth elements into the L1 domains. P-T constra ints (T > 800 degrees C, P > 6 kbar, a(H2O) similar to 0.3) suggest th at the leucosomes were formed through complete melting of biotite in f luid-absent conditions, following the model reaction Biotite + Alkali feldspar + Quartz reversible arrow Garnet + Ilmenite + Melt. The fract ion of melt generated during this process was low (<10 vol.%). The ide ntical size of the leucosomes as well as their homogeneous and isotrop ic distribution at outcrop scale, which lacks any evidence for melt se gregation, suggest that the migmatite remained a closed system. Subseq uent to migmatization, the leptynitic gneisses were intruded by garnet -bearing leucogranitic melts (L2), forming veins parallel and sub-perp endicular to the foliation. The leucogranites are rich in potassium (K 2O similar to 5.5 wt%), (Ba similar to 400 p.p.m.) and Sr (similar to 300 p.p.m.), and exhibit low concentrations of Zr (similar to 40 p.p.m .), Th (<1 p.p.m.) and Upsilon (<10 p.p.m.). The chondrite-normalized REE spectra show low abundances (La-N similar to 20, Lu-N similar to(3 )) and are moderately fractionated (La-N/Lu-N similar to 7). An Eu ano maly is absent or weakly negative. The higher Sr-87/Sr-86 ratio at 550 Ma (0.7345) compared with the migmatite (0.7164) precludes a direct g enetic relationship between leptynitic gneisses and leucogranites at M anali. Nevertheless, the chemical and mineralogical compositions of th e leuocogranites strongly favour a derivation through fluid-absent bio tite melting of isotopically distinct but chemically comparable Manali -type gneisses. The undersaturation of Zr, Th and REE, a typical featu re of leucogranitic melts generated during granulite facies anatexis o f psammo-pelitic lithologies and attributed to disequilibrium melting with incomplete dissolution of accessary phases (zircon, monazite), is weakly developed in the leucogranites of Manali. It is concluded that this is mainly due to the sluggish migration of the melts in static c onditions, which facilitated equilibration with the restitic gneisses.