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Pakistan Stratigraphy
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Cenozoic • Paleogene formation In GSP lexicon

Khadro Formation

Paleocene

Kirthar Basin · Eastern Kirthar (Sindh)

Part of Ranikot Group

Paleogene in the time scale →

Cited in 7 sources Last reviewed Jul 18, 2026

Unit summary
Rank
formation
Status
Published
Age
Cenozoic · Paleogene · PaleocenePaleocene
Named by
Williams (1959)
Type locality
Bara Nai, Lakhi Range26.1183°N, 67.8867°E
Thickness
In type section where at least two basaltic flows are present in the lower part, a thickness of 67 m is reported m
Lithology
Basal limestone with oysters and reptile bones, overlain by olive to grey ferruginous fossiliferous sandstone and gypsiferous shale with fossiliferous limestone interbeds; includes basaltic lava flows.
Synonyms
Not recorded

The bottom unit of the Paleocene Ranikot Group in Sindh — fossil-rich marine beds with early reptile bones and lava flows.

Named by Williams (1959) after Khadro Nai in the northern Laki Range (type section at Bara Nai), the Khadro Formation is the earliest-Paleocene unit of the Kirthar Basin and consists of limestone, sandstone, shale and volcanics — including Deccan-Trap basalt flows (the 'Khaskheli basalt') seen at surface and in the subsurface. It corresponds to the Cardita beaumonti beds of Blanford (1878). Its lower contact with the Vitakri Formation is disconformable and its upper contact with the Bara Formation is transitional and conformable. Earliest Paleocene.

Fossils

Contacts

In the Sindh Province column
SandstoneLimestoneFossils 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
marine
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

Not recorded

Remarks

The basal marine unit of the Paleocene Ranikot Group in the Kirthar/Sindh region, notable for reptile-bearing limestone and intercalated Deccan-related basaltic lava flows recording earliest-Cenozoic volcanism.

Sources (6)

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). Khadro Formation. In Pakistan Stratigraphy Dataset [Data set]. Zenodo. https://doi.org/10.5281/zenodo.21363991

BibTeX
@misc{stratigraphypk_khadroformation,
  author    = {Qudsi, Lareb},
  title     = {{Khadro 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/khadro-formation (accessed August 30, 2026).

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

    Saved on this device only.