Dharwar stratigraphy revisited: new age constraints on the 'oldest' supracrustal rocks of western Dharwar craton, southern India

• Published in: International geology review 2021-08, Vol.63 (12), p.1450-1470
• Main Authors: Patra, Kiranmala, Giri, Anshuman, Anand, R., Balakrishnan, S., Dash, Jitendra K.
• Format: Article
• Language: English
• Subjects: Age; Belts; Constraints; Cratons; Dharwar craton; Isotopes; Mesoarchaean; ophiolite; Rock; Rocks; Sargur Group; Stratigraphy; ultramafic rocks
• ISSN: 0020-6814; 1938-2839
• DOI: 10.1080/00206814.2020.1775138

The timing of emplacement of the oldest supracrustal rocks represented by Sargur Group is significant in understanding crustal evolution processes in the western Dharwar craton. The age of ultramafic-mafic rocks of the Sargur Group is not well-constrained as the komatiitic and komatiitic basaltic rocks have always given unreliable ages due to larger errors attributed to their alteration. New Sm-Nd isotope data from relatively less-altered layered intrusive ultramafic-mafic rocks of Nuggihalli and Holenarsipur greenstone belts of Sargur Group, western Dharwar craton give a much precise age of 2934 ± 88 Ma. This is the youngest age obtained for the ultramafic-mafic rock complexes of Sargur Group and is indistinguishable from the oldest ages reported for the overlying Dharwar Supergroup rocks. Sargur Group rocks might merely represent older ultramafic equivalents of the Dharwar Supergroup. A clear temporal distinction does not exist to support the stratigraphic classification of these two groups separately. However, the sub-contemporaneous to older ages obtained for the tonalite-trondhjemite-granodiorite gneisses that surround these greenstone belts would imply that the narrow belts tucked within the gneisses are younger, and therefore, the greenstone belts, whose dismembered roots and parts are exposed alongside the gneisses, could represent an Archaean analogue of an ophiolite suite.