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M. M. Singh
Bundelkhand University
Earth & Planetary Sciences Engineering Environmental Science Physics

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Geochemistry and tectonic setting of the supracrustal rocks from the central part of the Bundelkhand craton, India M. M. Singh; Vinod K. Singh
Journal of Geoscience, Engineering, Environment, and Technology Vol. 4 No. 2-2 (2019): Special Edition (Geology, Geomorphology and Tectonics of India)
Publisher : UIR PRESS

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (1056.942 KB) | DOI: 10.25299/jgeet.2019.4.2-2.2175

Abstract

Supracrustal rocks (mafics and ultramafics) occurs along with banded iron formation, and felsic volcanics around Babina, Dhaura, and Mauranipur linear east-west trends in central part of the Bundelkhand craton represent Archean crust. The mafic and ultramafic rocks geochemically classified into Komatiite and Basaltic Komatiite and have high-Fe Tholeiitic in composition which may relate with the primitive mantle. The major and trace element geochemistry of mafic and ultramafic rocks correspond to hydrated mantle with wedge tectonic sources and ocean ridge geological characteristics.
Co-Authors Vinod K. Singh