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Precambrian • Ediacaran In GSP lexicon

Salt Range Formation

Late Precambrian (Ediacaran)

Ediacaran in the time scale →

Cited in 11 sources Last reviewed Aug 20, 2026

Unit summary
Rank
Not recorded
Status
Published
Age
Precambrian · Ediacaran · EdiacaranLate Precambrian (Ediacaran)
Named by
Asrarullah (1967)
Type locality
Khewra, Salt Range, Punjab32.6486°N, 73.0111°E
Thickness
800-1500 m
Lithology
Rock salt (Billianwala Salt Member), gypsum (Bandar Kas Gypsum Member), marl (Sahwal Marl Member)
Synonyms
Punjab Saline Series; Saline Series

The oldest rocks exposed in the Salt Range: a thick Ediacaran sequence of rock salt, gypsum and marl formed when a restricted, evaporating sea dried out. It hosts the world-famous Khewra salt mine.

The oldest exposed formation in the Salt Range, consisting of evaporites deposited in a restricted marine environment. Contains the world-famous Khewra Salt Mine, second largest in the world. Includes Sahwal Marl Member, Bandar Kas Gypsum Member, and Billianwala Salt Member.

Fossils

Contacts

In the Salt Range column
Shale / mudGypsum / evaporiteFossils 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
restricted marine, evaporitic
Coordinates
32.6486°N, 73.0111°E

See it in the field

Geoheritage sites where this unit is exposed at outcrop.

Correlation

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

Economic significance

Major source of rock salt (Khewra Salt Mine), gypsum, and potential oil shales

Remarks

A late Neoproterozoic (Ediacaran) evaporite succession deposited under arid, restricted-marine conditions on the northwestern margin of the Indian Plate; geochemistry indicates felsic to intermediate source terrains. It forms the basal detachment of the Salt Range thrust belt and is the region's economic salt source.

Sources (11)

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

BibTeX
@misc{stratigraphypk_saltrangeformation,
  author    = {Qudsi, Lareb},
  title     = {{Salt Range 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/salt-range-formation (accessed August 30, 2026).

To cite the unit's original definition instead, see: Asrarullah (1967).

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