Primary sedimentary structures in the porcellanites of Panda Valley, Bhaunathpur, Lower Vindhyan Basin, district Garhwa (old Palamu), Jharkhand

Authors

  • Akhileshwar Tiwari P.G. Department of Geology, B.N. College, Patna University, Patna-6
  • V. S. Dube Department of Geology, Patna University, Patna-800005

DOI:

https://doi.org/10.3126/jngs.v26i0.32080

Keywords:

Sedimentary structures, Depositional environment, Pands valley, Lower Vindhyan Basin, Jharkhand

Abstract

Panda Valley consists of a thick pile of sediments in which there are three distinct Porcellanite horizons, Lower Porcellanite (LP), Middle Porcellanite (MP) and Upper Porcellanite (UP), with abundant sedimentary structures. The principle types of sedimentary structures noted in the Porcellanite Formation are discussed and an attempt has been made to interpret its depositional environment. The sedimentary structures are suggestive of deposition of sediments in low to moderately high energy, shallow to moderately deep waters in moderately stable tectonic environment.

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Published

2002-10-13

How to Cite

Tiwari, A., & Dube, V. S. (2002). Primary sedimentary structures in the porcellanites of Panda Valley, Bhaunathpur, Lower Vindhyan Basin, district Garhwa (old Palamu), Jharkhand. Journal of Nepal Geological Society, 26, 43–48. https://doi.org/10.3126/jngs.v26i0.32080

Issue

Vol. 26 (2002)

Section

Articles

License

© Nepal Geological Society