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1 Palaeoproterozoic Mineralization Research Group, Department of Geology, University of Johannesburg, Johannesburg 2006, South Africa
2 Department of Geology, Presidency College, Kolkata 700073, India
3 Department of Mineralogy, Technische Universität Bergakademie Freiberg, D-09596 Freiberg, Germany
4 Research School of Earth Sciences, Australian National University, Canberra, A.C.T. 0200, Australia
*Corresponding author (e-mail: hmrajesh{at}uj.ac.za)
Supplementary material: Representative major element, trace element and REE composition of the Dalli-Rajhara granite samples and a summary of SHRIMP U-Pb zircon data for the granite sample D-9 are available at http://www.geolsoc.org.uk/SUP18337.
Granitoids in the early Archaean are believed to be potassium-poor tonalite–trondhjemite–granodiorite rocks. Only after continental crust attained sufficient thickness did true (relatively potassium-rich) granites form. No record of true granite prior to 3.4 Ga is available. We report a 3.6 Ga true granite from the Archaean Bastar craton in India. In contrast to the typical early Archaean granitoids, which are commonly deformed into gneisses, this granite is relatively undeformed. The age and composition of the granite implies that continental crust of the Bastar craton attained sufficient thickness to permit intracrustal melting at 3.6 Ga.
