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Pakistan Stratigraphy
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Cenozoic • Paleogene formation In GSP lexicon

Sui Main Limestone Formation

Early Eocene (Ypresian) (Ypresian; ~56-52.83 Ma)

Paleogene in the time scale →

Cited in 6 sources Last reviewed Jul 30, 2026

Unit summary
Rank
formation
Status
Published
Age
Cenozoic · Paleogene · Early Eocene (Ypresian)Early Eocene (Ypresian) (Ypresian; ~56-52.83 Ma)
Named by
Not recorded
Type locality
Well Sui-36
Thickness
152-486 m
Lithology
Limestone. At its type section Sui Main Limestone is composed entirely of limestone with minor dolomite, calcareous shales and marls. The limestone is creamy white to dirty white to off white in color. It is firm to moderately hard, occasionally soft, sub blocky to blocky, micro to cryptocrystalline and chalky in parts. The proposed formation represents a rich bioclastic limestone. It consists mo…
Synonyms
Not recorded

Limestone. At its type section Sui Main Limestone is composed entirely of limestone with minor dolomite, calcareous shales and marls. The limestone is creamy white to dirty white to off white in color. It is firm to moderately hard, occasionally soft, sub blocky to blocky, micro to cryptocrystalline and chalky in parts. The proposed formation represents a rich bioclastic limestone. It consists mostly of fine grained lime wackstone, packstone and grainstone. Sedimentary structures are almost entirely of burrows, bioturbation and nodular bedding, although vugs occur rarely. Pyrite crystals are …

Fossils

Not recorded

Contacts

In the Sulaiman Fold Belt column
Shale / mudSandstoneLimestoneFossils 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
Not recorded
Region
Not recorded
Depositional environment
shallow marine, carbonate platform
Coordinates
Not recorded

Correlation

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

Economic significance

Major gas reservoir at the Sui, Kandhkot and related fields; named by PPL. Subsurface type section at Sui.

Remarks

The lower Eocene (Ypresian) Sui Main Limestone is the most prolific gas reservoir in Pakistan south of ~29°N, with more than 20 tcf of recoverable gas across 14 discovered fields (Siddiqui 2004). It does not outcrop anywhere in Pakistan and is known only in the subsurface; reservoir-quality carbonate development is restricted, diminishing northward as clastic influx increases toward the Sulaiman Range and the Jaisalmer basin.

Sources (5)

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

BibTeX
@misc{stratigraphypk_suimainlimestone,
  author    = {Qudsi, Lareb},
  title     = {{Sui Main Limestone 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/sui-main-limestone (accessed August 30, 2026).

    Saved on this device only.