Ultra‐high‐temperature metamorphism and multistage decompressional evolution of sapphirine granulites from the Palni Hill Ranges, southern India

Sapphirine granulites from a new locality in the Palni Hill Ranges, southern India, occur in a small enclave of migmatitic, highly magnesian metapelites (mg=85–72) within massive enderbitic orthogneiss. They show a variety of multiphase reaction textures that partially overprint a coarse‐grained high‐pressure assemblage of Bt+Opx+Ky+Grt+Pl+Qtz. The sequence of reactions as deduced from the corona and symplectite assemblages, together with petrogenetic grid considerations, records a clockwiseP–Tevolution with four distinct stages. (1) Equilibration of the initial high‐Passemblage in deep overthickened crust (12 kbar/800–900 °C) was followed by a stage of near‐isobaric heating, presumably as a consequence of input of extra heat provided by the voluminous enderbitic intrusives. During heating, kyanite was converted to sillimanite, and biotite was involved in a series of vapour‐phase‐absent melting reactions, which resulted in the ultra‐high‐temperature assemblage Opx+Crd+Kfs+Spr±Sil, Grt, Qtz, Bt, coexisting with melt (equilibration atc.950–1000° C/11–10 kbar). (2) Subsequently, as a result of decompression of the order of 4 kbar at ultra‐high temperature, a sequence of symplectite assemblages (Opx+Sil+Spr/Spr+Crd→Opx+Spr+Crd→Opx+Crd→Opx+Crd+Spl/Crd+Spl) developed at the expense of garnet, orthopyroxene and sillimanite. This stage of near‐isothermal decompression implies rapid ascent of the granulites into mid‐crustal levels, possibly due to extensional collapse and erosion of the overthickened crust. (3) Development of late biotite through back‐reaction of melt with residual garnet indicates a stage of near‐isobaric cooling toc.875 °C at 7–8 kbar, i.e. relaxation of the rapidly ascended crust to the stable geotherm. (4) A second period of near‐isothermal exhumation up toc.6–5 kbar/850 °C is indicated by the partial breakdown of late biotite through volatile phase‐absent melting reactions. Available isotope data suggest that the early part of the evolutionary history (stages 1–3) is presumably coeval with the early Proterozoic metamorphism in the extended granulite terrane of the Nilgiri, Biligirirangan and Shevaroy Hills to the north, while the exhumation of the granulites from mid‐crustal levels (stage 4) occurred only during the Pan‐African thermotectonic event, which led to the accretion of the Kerala Khondalite Belt to the south.