Neoarchean clockwise P-T trajectories with evolution sequence from HP to UHT metamorphism during decompression: Evidence from petrology, mineralogy, and phase equilibria modeling of mafic granulites in the Sittampundi Complex, southern India

The dispute of tectonic environments such as subduction-collision setting versus extension tectonic setting, is a common phenomenon in the Precambrian. Despite the ongoing controversy, the pressure-temperature ( P - T ) paths recorded by metamorphic rocks are often used as an indicator for distinguishing between subductioncollision and extension tectonic settings in the early Precambrian. It is widely acknowledged that highpressure (HP) granulites may have formed in crustal -thickening -dominated collision/subduction environment. Conversely, ultra -high temperature (UHT) granulites may have formed in the elevated mantle heat flux environment. The Sittampundi Complex (SC), where HP granulites and UHT granulites coexist, plays a crucial role in unraveling the late-Neoarchean to early-Paleoproterozoic tectonic evolution of northern South Granulite-facies Terrane (NSGT) of India. In this study, we present new P - T paths from three HP mafic granulites overprinted by UHT granulite facies metamorphism in the SC and provide more data to unravel metamorphic evolution of NSGT. Phase equilibria modeling and traditional thermobarometry calculations illustrated that clockwise metamorphic pressure-temperature ( P - T ) paths were yielded, passing from 3.3 to 9.3 kbar/631-669 degrees C (prograde stage) through 11.9-18.5 kbar/828-986 degrees C (pressure -peak stage), and through 6.6-11.1 kbar/ 1019-1085 degrees C (temperature -peak stage) to 4.4-8.1 kbar/845-930 degrees C (retrograde stage). The HP mafic granulites exhibit clockwise P - T paths with a considerable heating process (ca. 150-180 degrees C) from the pressure -peak stage (HP -granulite sub-facies) to the temperature -peak stage (UHT -granulite sub-facies). Zircon U-Pb dating yields an age of 2513 +/- 29 indicates that the metamorphism took place in the Neoarchean. The uncommon P - T paths from Neoarchean HP granulite in the NSGT suggest that during late Neoarchean, the NSGT had experienced the crustal -thickening dominated collision/subduction (assembly of micro -blocks of Dharwar Craton) and subsequently mantle diapirism process.