Title : The Evolution of Granite-Greenstone Belts of the Western part of Dharwar Craton, Dharwar Craton, South India

Abstract

The evolution of granite-greenstone belts within the Western Dharwar Craton (WDC), a Paleoarchean-Neoarchean crustal accretion, represents the major Archean records of Early Earth. In this contribution, an integrating field relationships-whole-rock geochemistry (major/trace elements, REE patterns), and isotope systematics (Sm-Nd, Lu-Hf) depict an initial TTG-komatiite formation at 3400-3300 Ma linked to juvenile mantle inputs and elevated geothermal gradients, and a mixed tectonic setup. Subsequently, the dome-and-keel architectures emerge through subduction and plume tectonics represented by Sargur Group volcanics (~3.3 Ga), indicating high mantle potential temperatures and distinct tectonic manifestation of Archean Earth. While the younger Bababudan (~2.9 Ga) and Chitradurga (~2.7 Ga) greenstones hosting volcano-sedimentary assemblages reflect back-arc volcanism atop stabilised TTG basement, with two phases of 3.0Ga and 2.6 Ga. The Isotopic U-Pb zircon and radiogenic isotope data reveal episodic crustal growth, contrasting WDC's stable, thick (~42-51 km) core with major growth events at 3.35-3.25Ga, including TTG and Komatiitic Volcanism. Vertical tectonics dominate over nascent subduction, underscoring plume-driven nucleation of proto-cratons globally. Therefore, the eventual formation of granite greenstone belts of Western Dharwar Craton from a wide early Earth time window and proxies to investigate the sequential evolution of Archean cratonic units.