Abstract
Evidences of Large-Scale Shearing from South-Eastern Extension of The Mahakoshal Belt, Covering Parts of Sidhi & Singrauli Districts of Madhya Pradesh and Sonbhadra District, Uttar Pradesh, India
Highlights
The Mahakoshals have a WNW-ESE trending arm in the south-eastern corner, especially south of Chitrangi
Overwhelming presence of anticlockwise rotated fabric elements, producing S-C structure in phyllite/ phyllonite and in meta-greywacke, along with frequent presence of ‘alpha’ and ‘delta’ type structures, strongly asymmetric ‘S’ and at places ‘Z’ shaped folds and the sheath folds suggest that the ductile shearing with a sinistral shear sense is spread over the entire WNW trending sinuous arm of Mahakoshals
Sharma [7], has reported the presence of turbidites restricted within the WNW trending arm of the Mahakoshals
Summary
Evidences of Large-Scale Shearing from South-Eastern Extension of The Mahakoshal. Belt, Covering Parts of Sidhi & Singrauli Districts of Madhya Pradesh and Sonbhadra. How to cite this article: Banerji DC. Evidences of Large-Scale Shearing from South-Eastern Extension of The Mahakoshal Belt, Covering Parts of Sidhi & Singrauli Districts of Madhya Pradesh and Sonbhadra District, Uttar Pradesh, India.
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