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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 recordedContact not recorded

Band colour = period; texture = dominant rock type. Lines between bands mark the contact type; dotted = no contact recorded in the sources (not a claim of conformity). 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.

Research notes (6)

Field-by-field findings drawn from the cited literature. Every statement is traced to a registered source — follow a citation for the full reference.

Name & nomenclature (1)

  • Attested in Shah (2009), Geological Survey of Pakistan Memoir 22 - the Stratigraphic Committee of Pakistan's compiled lexicon (listed in the memoir's contents). Adds the definitional GSP/SCP lexicon citation.

    Shah, S.M.I. (2009)

Age & correlation (1)

  • Afzal, Williams & Aldridge (2009) treat the Bara Formation (Shah 1977) as the lower sandstone/siltstone part of the Dungan Formation; it lacks age-diagnostic fossils (Shah 1977; Afzal 1996; Wakefield & Monteil 2002) and its Paleocene age rests on stratigraphic position between the P1 Khadro and the late Thanetian-early Ilerdian upper Dungan. Supports the curated Paleocene age.

    Afzal, J., Williams, M. & Aldridge, R.J. (2009)

Economic significance (3)

  • Malik (1989): the mid-Paleocene Bara Formation (dominantly sandstone over Khadro basaltic lava flows, near Kalri Lake) hosts the Sonda coalfield of the Lower Indus Basin - eleven coal seams, three workable, with a cumulative 4-6 m and reserves ~500 Mt (9,599-12,743 BTU/lb); the coal is rich in fixed carbon and sulphur.

    Malik, I.A. (1989)

  • Wnuk et al. (1993, USGS OFR 93-256): although the Paleocene Bara Formation is the principal coal-bearing unit of the Lower Indus Basin (worked historically NW of the Lakhra Anticline), a coal-resource assessment at Fort Ranikot in the northern Lakhi Range found NO coal in the Bara rocks there - the coal beds are absent or structurally obscured at that locality. A documented negative result that bounds the field's coal distribution.

    Wnuk, C., Sanfilipo, J.R., Chandio, A.H. & Fatmi, S.F. (1993)

  • Coal-resource assessment of the Paleocene Bara Formation (Ranikot Group) in the Fort Ranikot area, northern Lakhi Range, Sindh, documents its fluviatile-to-paralic coal-bearing succession — part of the Lakhi Range / Sonda-Thatta Sindh coalfields (Wnuk et al. 1993).

    Wnuk, C., SanFilipo, J.R., Chandio, A.H. & Fatmi, S.F. (1993)

Geological significance (1)

  • Malkani (2016) describes the Paleocene Bara Formation of the Kirthar (lower Indus) Basin as sandstone with minor limestone, coal and volcanics, the latter attributed to Deccan volcanism near the K/Pg boundary.

    Malkani, M.S. (2016)

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.

Spotted an error? Suggest a sourced correction →

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 October 29, 2026).

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

    Saved on this device only.