Grenville-age Metamorphism in the Larsemann Hills: P-T Evolution of the Felsic Orthogneiss in the Broknes Peninsula, East Antarctica

The gneisses outcropping in the Larsemann Hills of East Antarctica are ideal for studying the composition and evolution of the Prydz tectonic belt. In this study, detailed petrological analyses, phase equilibrium modelling, and zircon analyses were performed on a felsic orthogneiss from the Broknes Peninsula in the Larsemann Hills. The study results show that the protolith of the felsic gneiss is granite, which is further identified to have been an S-type granitoid. The felsic orthogneiss intruded into the basement complex at similar to 976 Ma. The magmatic zircons in the felsic orthogneiss have lower LREE and higher HREE contents than those of the metamorphic zircons in the same rock. The felsic gneiss consists of the mineral assemblage garnet + ilmenite + plagioclase + K-feldspar + sillimanite + quartz and underwent granulite facies metamorphism in the Grenvillian period (similar to 899 Ma), with peak conditions of similar to 870 degrees C and similar to 9.5 kbar. The Larsemann Hills should be categorized as the orogenic process from arc-continent collision to continent-continent collision during the Grenvillian period, crust thickening(similar to 899 Ma) and subsequent collapse(550-500 Ma).