Evidences of Multiple Deformations Near Amaidegri in the Western Part of the Gangpur Group

Authors

  • Department of Geology and Geophysics, Indian Institute of Technology, Kharagpur-721302
  • Department of Geology and Geophysics, Indian Institute of Technology, Kharagpur-721302
  • Department of Geology and Geophysics, Indian Institute of Technology, Kharagpur-721302

Abstract

Three phases of folding have been detected in a large exposure along the Sapai lladi near Amaidegri (22°01': 84°08') in the Ghoriajhor manganese belt in the western part of the Gangpur Group. Reclined to inclined folds (F1) plunging SSE have been coaxially refolded by open upright F2 folds, and finally, upright folds with ENE-trending axial planes (F3) cause culmination and depression of axes of open-folded reclined folds. The multiple deformations cause characteristic outcrop patterns and they are reflected in two distinct S-pole girdles around a plane of symmetry which is the axial trend of F3 folds.

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Research Papers

Published

1980-12-01

How to Cite

Chaudhuri, A. K., Pal, A. B., & Roy, A. (1980). Evidences of Multiple Deformations Near Amaidegri in the Western Part of the Gangpur Group. Journal of Geological Society of India, 21(12), 617–622. Retrieved from https://geosocindia.com/index.php/jgsi/article/view/64917

References

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CHAUDHURI, A. K. and BARUA, S. K., (1976) Structure of the Dublabera Fold at the core of Gangpur Series in Orissa, India. Indian Jour. Earth. Sci., v. 3, pp. 21-25.

CHAUDHURI, A. K. and PAL, P. K., (1976) Deformed pebbles in the Raghunathpalli conglomerate near Rourkela, Orissa, India. Indian Jour. Earth Sci .. v. 3, pp. 160-167.

CHAUDHURI, A. K. and PAL, A. B., (1977) Superposed folding in the northern part of the Gangpur Series, Orissa. Jour. Ceol. Soc. India, v. 18, pp. 233-239.

CHAUDHURI, A. K. and PAL, A. B., (1979) Pebble strain analysis in the Raghunathpalii conglomerate of Gangpur Group Orhsa, India. Jour. Geol. Soc. India (in press).

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