Significant palynozones of Subathu Formation (Himachal Pradesh) and their bearing on stratigraphy

H.P. Singh; Samir Sarkar

doi:10.54991/jop.1986.1537

Significant palynozones of Subathu Formation (Himachal Pradesh) and their bearing on stratigraphy

Authors

H.P. Singh Birbal Sahni Institute of Palaeobotany, 53, University Road, Lucknow 226007, India
Samir Sarkar Birbal Sahni Institute of Palaeobotany, 53, University Road, Lucknow 226007, India

DOI:

https://doi.org/10.54991/jop.1986.1537

Keywords:

Palynostratigraphy, Correlation, Subathu Formation, Palaeocene-Eocene (India)

Abstract

The distribution of the Subathu Formation palynozones (Upper Palaeocene-Upper Eocene) in the area of Kalka-Simla and Banethi-Bagthan (Himachal Pradesh) has been discussed. The comparative study of these palynozones shows that they are correlatable which has been inferred from the evidence of lateral distribution of the Subathu assemblages studied from widely separated areas.

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Published

1986-12-31

How to Cite

Singh, H., & Sarkar, S. (1986). Significant palynozones of Subathu Formation (Himachal Pradesh) and their bearing on stratigraphy. Journal of Palaeosciences, 35((1-3), 249–257. https://doi.org/10.54991/jop.1986.1537