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Pakistan Stratigraphy
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Cenozoic • Neogene formation GSP memoir

Talar Formation

Late Miocene (Messinian; ~6.7-5.3 Ma)

Balochistan Basin · Makran-Siahan Basin, Wazhdad Arc And Mashkel/Kharan Basin

Neogene in the time scale →

Cited in 6 sources Last reviewed Jul 31, 2026

Unit summary
Rank
formation
Status
Published
Age
Cenozoic · Neogene · Late MioceneLate Miocene (Messinian; ~6.7-5.3 Ma)
Named by
HSC (1961)
Type locality
Makran Flysch Province, Balochistan Basin25.9842°N, 62.5113°E
Thickness
not less than 5000 m
Lithology
Clayey sandstone; sandstone, shale and mudstone.
Synonyms
Hinglaj Group (in part)

A Miocene–Pliocene shallow-marine sandstone capping the Makran sequence — a potential reservoir.

Talar Formation is named after the Talar gorge (31 K/10; HSC, 1961). It is considered equilent to Hinglaj group of HSC (1961). It consists of sandstone, shale, mudstone and shelly limestone. Its lower contact with Parkini and Chatti formations is transitional but at places sharp. The fossils like gastropods (Mollusks) and lamellibranches are common. The microforms are Miocene age diagnostic (HSC 1961). The age of the formation is Late Miocene to Early Pliocene.

Fossils

Not recorded

Contacts

In the Makran Coast column
Shale / mudSandstoneFossils 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
Balochistan Basin
Region
Makran-Siahan Basin, Wazhdad Arc And Mashkel/Kharan Basin
Depositional environment
shallow marine, shelf
Coordinates
25.9842°N, 62.5113°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

A potential shallow RESERVOIR unit of the Makran, with stacked sandstones above the deeper turbidite reservoirs.

Remarks

A Miocene–Pliocene shallow-marine sandstone capping the regressive Makran succession, recording the final shoaling of the accretionary wedge to near sea level.

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: Appears in a single-author Geological Survey of Pakistan memoir (Malkani & Mahmood 2017), not cross-confirmed against the Shah lexicon. The Stratigraphic Committee of Pakistan is largely inactive, so documented provenance — not formal ratification — is the available signal.

Cite this unit
APA

Qudsi, L. (2026). Talar Formation. In Pakistan Stratigraphy Dataset [Data set]. Zenodo. https://doi.org/10.5281/zenodo.21363991

BibTeX
@misc{stratigraphypk_talarformation,
  author    = {Qudsi, Lareb},
  title     = {{Talar 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/talar-formation (accessed September 5, 2026).

To cite the unit's original definition instead, see: HSC (1961).

    Saved on this device only.