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Pakistan Stratigraphy
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Mesozoic • Cretaceous formation In GSP lexicon

Moro Formation

Late Cretaceous (Maastrichtian) (Maastrichtian; ~70.02-67.88 Ma)

Cretaceous in the time scale →

Cited in 6 sources Last reviewed Aug 2, 2026

Unit summary
Rank
formation
Status
Published
Age
Mesozoic · Cretaceous · Late Cretaceous (MaastrichtianLate Cretaceous (Maastrichtian) (Maastrichtian; ~70.02-67.88 Ma)
Named by
Hunting Survey Corporation (1960)
Type locality
Moro River section in Kirthar Range, between Johan and Bibi Nani
Thickness
~110–140 m
Lithology
Pelagic marl. It consists of grey, medium to thick bedded, grey to dark grey marl, dark grey to grey green calcareous shale and minor sandstone and volcanic conglomerate of mottled appearance (only in the lower part). Limestone is the dominant lithology in the Sulaiman Province where it contains chert lenses, while marl is dominant in Sanjawi area (Sulaiman Province) and the Axial Belt. In the Ki…
Synonyms
Not recorded

Pelagic marl. It consists of grey, medium to thick bedded, grey to dark grey marl, dark grey to grey green calcareous shale and minor sandstone and volcanic conglomerate of mottled appearance (only in the lower part). Limestone is the dominant lithology in the Sulaiman Province where it contains chert lenses, while marl is dominant in Sanjawi area (Sulaiman Province) and the Axial Belt. In the Kirthar Province, shale constitutes the main rock type. The formation is recognized in the Sulaiman and Kirthar provinces and the Axial Belt. It conformably overlies Pab Sandstone Fm; where Pab is not d…

Fossils

OrbitoidesOrbitellabivalvesbrachiopodsgastropods

Contacts

In the Sindh Province column
LimestoneMarlIgneousFossils recordedConformableUnconformity

Band colour = period; texture = dominant rock type. Lines between bands mark the contact type (wavy = unconformity inferred from a missing period). 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
Not recorded
Region
Not recorded
Depositional environment
shallow marine, open shelf
Coordinates
Not recorded

Correlation

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

Economic significance

Not recorded

Remarks

A Maastrichtian fossiliferous limestone-and-shale unit of the Kirthar–Sulaiman belt, the local uppermost-Cretaceous marine record. It rests disconformably (oxidised erosional contact, basal conglomerate) on the Parh Limestone or Fort Munro Formation and is conformably overlain by the Pab Formation in the Spera Ragha–Chinjun area.

Sources (6)

Reviewer confidence: medium

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

BibTeX
@misc{stratigraphypk_moroformation,
  author    = {Qudsi, Lareb},
  title     = {{Moro 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/moro-formation (accessed August 30, 2026).

To cite the unit's original definition instead, see: Hunting Survey Corporation (1960).

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