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Mesozoic • Triassic formation In GSP lexicon

Wulgai Formation

Triassic

Kirthar Basin · Western Kirthar (Balochistan)

Part of Khanozai Group

Triassic in the time scale →

Cited in 6 sources Last reviewed Aug 2, 2026

Unit summary
Rank
formation
Status
Published
Age
Mesozoic · Triassic · TriassicTriassic
Named by
Williams (1959)
Type locality
Tarkai-Gwal section, Axial Belt
Thickness
180 m
Lithology
Indurated dark-grey mudstone and shale with intercalations of thin limestone, calcareous mudstone and sandstone.
Synonyms
Alozai Group / Shirinab Formation / Winder Group (earlier mappings, HSC 1960); Wulagai

A Triassic dark mudstone-and-shale, the base of the Mesozoic sequence in western Balochistan.

Wulgai Formation Wulgai is named by Williams 1959 after Wulgai village for variegated shale with medium bedded limestone of Middle to Late Triassic age exposed in the Western Indus Suture regions like Shirinab area of Mastung and Kalat, Khanozai, Zhob, etc. It is 180 m thick in the Trakai-Gwal section. Its lower contact with Gwal is sharp with fossiliferous conglomeratic and dense limestone and upper contact with Spingwar formation seems to be conformable. The fossils like radiolarian, conodonts and some Spiriferinid brachiopods in basal limestone indicates Middle Triassic age and Holobia, 70 Daonella (Bivalves) and ammonites like Cladescites, Jovites, Arietoceltites, Anatomites, Juvavites, Arcetes indicating Late Triassic.

Fossils

Contacts

In the Kirthar Range column
Shale / mudLimestoneFossils 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
Western Kirthar (Balochistan)
Depositional environment
marine
Coordinates
Not recorded

Correlation

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

Economic significance

Part of the frontier Triassic–Jurassic carbonate petroleum play of the Sulaiman Fold-Thrust Belt; dolomitization of the Wulgai Formation carbonates has locally produced secondary porosity.

Remarks

A Triassic mudstone-shale unit of the Balochistan ophiolite-and-thrust belt (Zhob, Kalat, Khuzdar), also encountered in Lower Indus wells; the base of the Mesozoic succession there.

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

BibTeX
@misc{stratigraphypk_wulgaiformation,
  author    = {Qudsi, Lareb},
  title     = {{Wulgai 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/wulgai-formation (accessed August 30, 2026).

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

    Saved on this device only.