Study of a Deformed Conglomerate Horizon in the Sandur Schist Belt, Bellary District, Karnataka

Authors

  • Abhinaba Roy
     Jayanagar, Bangalore-560011
  • Debashish Ghosh
     Cement Research Institute of India, New Delhi-110048

Abstract

The deformed pebbles of the conglomerate horizon occurring to the SE of Hospet have their longest and the intermediate axis lying on the schistosity plane. The long axis shows a strong preferred orientation. The intermediate axis is parallel or subparallel to the regional fold axis. The strain is plane strain type with slight elongation parallel to the intermediate axis or the regional fold axis.

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Issue

Volume 20, Issue 7, July 1979

Section

Research Notes

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Published

1979-07-01

How to Cite

Roy, A., & Ghosh, D. (1979). Study of a Deformed Conglomerate Horizon in the Sandur Schist Belt, Bellary District, Karnataka. Journal of Geological Society of India, 20(7), 349–352. Retrieved from https://geosocindia.com/index.php/jgsi/article/view/64449

References

DUNNET, D., (1969) A technique of finite strain analysis using elliptical particles. Tectonophysics, v, 7, pp. 117-136.

ELLIOT, D., (1970) Determination of finite strain and initial shape from deformed elliptical objects. Geol. Soc. America Bull., v. 81, pp. 2221-2236.

M1SHRA, R. N., (1972) Systematic mapping in Sandur schist belt, GSI, report, (unpublished.)

MUKHOPADHYAY, D., (1973) Strain measurements from deformed quartz grains in slaty rocks from the Ardennes and the northern Eifel. Tectonophysics. v. 16, pp. 279-296.

RAMSAY, J. G., (1967) Folding and Fracturing of Rocks. McGraw-Hili, New York, N.Y. 568 p.

ROY, A. and BISWAS, S. K., (1977) Geology of parts of Hospet, Sandur and Bellary taluks, Bellary district, Karnataka, GSI, report, (unpublished).

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