The Spiti Ordovician-Silurian Succession

Authors

  • R. K. Goel
     Dept. of Geology & Geophysics, University of Roorkee
  • N. G. K. Nair
     Dept. of Geology & Geophysics, University of Roorkee

Abstract

Classic pin valley section in Spiti (Himachal Pradesh) India, has been re-examined and formal stratigraphic nomenclature in terms of the Lower Paleozoic succession of Spiti is proposed.

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Issue

Volume 18, Issue 1, January 1977

Section

Research Notes

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Published

1977-01-01

How to Cite

Goel, R. K., & Nair, N. G. K. (1977). The Spiti Ordovician-Silurian Succession. Journal of Geological Society of India, 18(1), 47–48. Retrieved from https://geosocindia.com/index.php/jgsi/article/view/63764

References

BOUCOT, A. J. and GAURI. K. L., (1968) Age and Relationship of Basal Muth Quartzite of Kashmir, India. Geol. Soc. Am. (Abst.). p. 33.

DASGUPTA, P. K .. (1971) On textural characteristics of the Muth Quartzite of Spiti and Kuti regions, Central Himalayas. Jour. Geol. Soc. India. v. 12 (2), pp. 152-158.

GUPTA, V. J., (1973) Indian Paleozoic Stratigraphy, p. 204, Hindustan Publishing Corporation, New Delhi.

HAYDEN, H. H., (1904) Geology of Spiti with parts of Bashahr and Rupshu. Mem. Geol. Surv. India, v. 36 (1), pp. 1-129.

REED, F. R. C., (1912a) Ordovician and Silurian fossils of Central Himalayas. Pal. Ind. Geol. Surv. India. Ser 15, v. 7 (2), pp. 1-168.

REED, F. R. C., (1912b) Silurian fossils from Kashmir. Pal. Ind. Geol. Surv. India. v. 42 (1), pp. 16-33.

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