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Cenozoic • Paleogene formation In GSP lexicon

Bara Formation

Paleocene

Kirthar Basin · Eastern Kirthar (Sindh)

Part of Ranikot Group

Paleogene in the time scale →

Cited in 10 sources Last reviewed Aug 9, 2026

Unit summary
Rank
formation
Status
Published
Age
Cenozoic · Paleogene · PaleocenePaleocene
Named by
Williams (1959)
Type locality
Bara Nai, northern Laki Range26.1183°N, 67.8867°E
Thickness
60-600 m (based on surface exposures) m
Lithology
Fluviatile to paralic sandstone and shale with coal and carbonaceous beds.
Synonyms
Not recorded

The coal-bearing middle unit of the Paleocene Ranikot Group — the source of Sindh's coal.

Named by Ahmad and Ghani (in Cheema et al., 1977) after Bara Nai in the Laki Range, with its principal reference section at Ranikot, the Bara Formation consists of soft sandstone, shale and coal. It corresponds to the lower Ranikot sandstone of Vredenburg (1906) and the equivalents of later workers. Its lower contact with the Khadro Formation and upper contact with the Lakhra Formation are transitional and conformable. Age: Early Paleocene.

Fossils

Not recorded

Contacts

In the Sindh Province column
LimestoneSandstoneFossils recordedConformable

Band colour = period; texture = dominant rock type. Lines between bands mark the contact type. True scale makes height ∝ recorded thickness; hatched = thickness not recorded. Ages approximate, for ordering.

This unit (highlighted) within its province column; faded ends continue above and below. Line style marks the contact type.

Distribution & setting

Basin
Kirthar Basin
Region
Eastern Kirthar (Sindh)
Depositional environment
fluvial, paralic
Coordinates
26.1183°N, 67.8867°E

See it in the field

Geoheritage site where this unit is exposed at outcrop.

Correlation

Not recorded. Compare this unit against other basins on the correlation panel →

Economic significance

The principal coal-bearing horizon of the Sindh (Lower Indus) coalfields, including the Lakhra, Sonda and Thar areas.

Remarks

The middle, coal-bearing fluvio-paralic unit of the Paleocene Ranikot Group and the main coal horizon of the Sindh coalfields.

Sources (10)

Reviewer confidence: high

Every fact on this page is source-cited. This entry is part of the peer-archived Pakistan Stratigraphy Dataset (doi.org/10.5281/zenodo.21363991, CC‑BY‑4.0).

Lexicon status: Name attested in the Shah (1977/2009) Geological Survey of Pakistan compilation — the national stratigraphic lexicon. This records where the name is documented; it is not an endorsement of the unit’s definition, age or figures.

Cite this unit
APA

Qudsi, L. (2026). Bara Formation. In Pakistan Stratigraphy Dataset [Data set]. Zenodo. https://doi.org/10.5281/zenodo.21363991

BibTeX
@misc{stratigraphypk_baraformation,
  author    = {Qudsi, Lareb},
  title     = {{Bara Formation} --- Pakistan Stratigraphy Dataset},
  year      = {2026},
  publisher = {Zenodo},
  doi       = {10.5281/zenodo.21363991},
  url       = {https://doi.org/10.5281/zenodo.21363991}
}

Archived dataset: doi.org/10.5281/zenodo.21363991 (CC‑BY‑4.0) · Direct link to this entry: https://stratigraphy.pk/formation/bara-formation (accessed September 5, 2026).

To cite the unit's original definition instead, see: Williams (1959).

    Saved on this device only.