Evidences of Three Phases of Deformation in the Pre-Cambrian Rocks of Raisindri Pahar, Singhbhum, Bihar

Authors

  • S. Pasayat
     Department of Geology and Geophysics, Indian Institute of Technology, Kharagpur, West Bengal
  • D. S. Bhattacharyya
     Department of Geology and Geophysics, Indian Institute of Technology, Kharagpur, West Bengal

Abstract

Earlier workers recognised two phases of deformation. Evidences are presented here which indicate three phases of deformation. The imprint of the last phase of deformation is strongest.

Downloads

Download data is not yet available.

Metrics

Metrics Loading ...

Issue

Volume 18, Issue 4, April 1977

Section

Research Notes

Downloads

Published

1977-04-01

How to Cite

Pasayat, S., & Bhattacharyya, D. S. (1977). Evidences of Three Phases of Deformation in the Pre-Cambrian Rocks of Raisindri Pahar, Singhbhum, Bihar. Journal of Geological Society of India, 18(4), 198–202. Retrieved from https://geosocindia.com/index.php/jgsi/article/view/63790

References

BATTACHARYYA, D. S., (1966) Structure of the rocks of the Sonapet Valley, Singhbhum dist., Bihar. Bull. Geol. Mill Met. Soc. India, no. 36.

BATTACHARYYA, D. S. and. PASAYAT, S., (1971) Structure of the rocks around Nakti-Ghagra, Singhbhum dist., Bihar. Quart. Jour. Geol. Mill. Met. Soc. India, v. 43, no. 3, pp. 149-151.

DUNN, J. A., (1929) The Geology of North Singhbhum etc. Mem, Geol, Surv, India, v. 54.

SARKAR, S. N. and A. K. SAHA, (1962) A revision of Precambrian stratigraphy and tectonics of Singhbhum etc. Quart, Jour. Geol, Mill. Met. Soc. India, v. 34, no. 2-3, pp. 97-136.