Petrology of the Siliciclastic Rocks Around Surgutaria (S.E. of Joda) Keonjhar District, Orissa

Authors

  • S. K. Ghosh
     Department of Geology, Banaras Hindu University, Varanasi-22I 005
  • B. K. Chatterjee
     Department of Geology, Banaras Hindu University, Varanasi-22I 005

Abstract

Siliciclastic rocks around Surgutaria viIIage are mature to sub-mature quartzarenites to quartz-wackes, Quartz-wackes are produced due to extensive readjustment of sericite-chert matrix during phyllomorphic stage of development in the arenite frame work. Various statistical parameters, and current structures clearly reveal that the deposition of siliciclastics took place in a stable shallow marine to tidal flat environment.

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Issue

Volume 24, Issue 6, June 1983

Section

Research Notes

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Published

1983-06-01

How to Cite

Ghosh, S. K., & Chatterjee, B. K. (1983). Petrology of the Siliciclastic Rocks Around Surgutaria (S.E. of Joda) Keonjhar District, Orissa. Journal of Geological Society of India, 24(6), 314–317. Retrieved from https://geosocindia.com/index.php/jgsi/article/view/65363

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