G. Gietelink. (1978). A prominent shear zone runs E-W across Singhbhum. Structural analysis indicates three phases of folding, all with E-W axial planes dipping northerly or subvertically to the north of the shear zone. South of this shear zone there are two phases of folding . Netherlands Journal of Geosciences, 65-76. Retrieved from https://njgjournal.nl/index.php/njg/article/view/14061