Metamorphic P–T evolution of Hercynite-quartz-bearing granulites from the Diwani Hill, North East Gujarat (NW India).

• Hercynite-quartz-bearing granulites occur on the southern tip of the South Delhi Terrane, India. • Preserved metamorphic reaction microstructures are indicative of a decompression event. • New SHRIMP data provide evidence for a Neoproterozoic age as a time of metamorphic overprint. • South Delhi basin would have been a remnant of the proto-Mozambique Ocean in NW India. Diwani Hill granulites occurring on the southern tip of the South Delhi Terrane (SDT) of Aravalli Mobile Belt (AMB), comprises rocks of granulite facies and represent the deeper level of the crust. The SDT represents an admixture of charnockites, granites, calc-granulites and hercynite-quartz-bearing pelitic granulites. The symplectite and corona textures recorded in the hercynite-quartz-bearing granulites from a part of SDT provides a wide spectrum of P-T sensors in support of the petrological evolution. P-T evolution of these hercynite-quartz-bearing granulites has been constrained through the use of THERMOCALC program, conventional thermobarometry, and pseudosection modelling in the NCKFMASHTO model system using Perple_X software. The unification of these three calculations, demonstrates that the hercynite-quartz-bearing granulites experienced peak pressure and temperature at 6.7 kbar and 750 °C, respectively. The textural imprints, multistage reaction textures, P-T pseudosections as well as the application of multi-equilibrium calculation give evidence for decompressive history related to their exhumation. SHRIMP U-Pb chronological results yield ages between 780 and 680 Ma as a time of metamorphic overprint, and the ages between 1591 and 1216 Ma corresponding with detritus derived from magmatic source for hercynite-quartz-bearing granulites. Zircon ages reflect that continental crust in the SDT resulted from the Mesoproterozoic protolith of an igneous origin whereas sedimentary succession was deposited between 1216 and 780 Ma. The present study envisages that the South Delhi basin would have been a remnant of the proto-Mozambique Ocean in NW India which was closed due to subduction. This subduction metamorphosed the sediments of the basin to granulite facies and the rocks were subsequently, uplifted because of the thrust sheet tectonics during the Neoproterozoic times. [ABSTRACT FROM AUTHOR]