Skip to content
Pakistan Stratigraphy
Suggest a correction
Paleozoic • Devonian formation Literature

Vandanil Formation

Early Devonian (Pragian)

Karakoram-Hindukush Basin · Central Karakoram Batholith

Devonian in the time scale →

Cited in 2 sources Last reviewed Jul 30, 2026

Unit summary
Rank
formation
Status
Published
Age
Paleozoic · Devonian · Early DevonianEarly Devonian (Pragian)
Named by
Gaetani et al. (2008)
Type locality
Type section on the southeast side of the Ribat Bar, above the summer meadows of Vandanil, Karambar Unit; recognized only in the Karambar Unit.
Thickness
about 625 m
Lithology
About 625 m in five lithozones: (1) grey slightly dolomitized limestone with crinoids, brachiopod and tabulate-coral fragments (~135 m); (2) light grey dolostones (~50 m); (3) grey carbonatic siltstones with nodular limestones and dolostone banks, capped by calcareous slates (~150 m); (4) grey nodular limestones rich in brachiopods, corals, crinoids and nautiloids (~120 m); (5) grey dolostones with massive mounds built by dendroid-to-phacelloid rugosans, tabulates and calcareous algae (~170 m).
Synonyms
Not recorded

The Vandanil Formation is an Early Devonian (Pragian) carbonate-ramp succession about 625 m thick, recognised only in the Karambar Unit of the Karakoram, where it forms the thickest and most complete Devonian–Carboniferous section of the range. Five lithozones grade from high-energy bioclastic limestones through sheltered nodular limestones and slates to a coral–algal mound at the top; conodonts (Pandorinellina steinhornensis miae and others, identified by R. Mawson) date it to the Pragian. It overlies the Ordovician Vidiakot slates and is overlain by the peritidal Chilmarabad Formation.

Fossils

Conodonts (Pandorinellina steinhornensis miae, Ozarkodina spp., Amydrotaxis spp.)CrinoidsBrachiopodsTabulate coralsRugosansCalcareous algaeNautiloids

Contacts

Lower contact — conformable; upper contact — conformable.

In the Hindukush-Chitral column
LimestoneMetamorphicMixedFossils 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
Karakoram-Hindukush Basin
Region
Central Karakoram Batholith
Depositional environment
marine, carbonate ramp
Coordinates
Not recorded

Correlation

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

Economic significance

Not recorded

Remarks

A Pragian (Early Devonian) carbonate ramp in the Karambar Unit, the thickest and most complete Devonian–Carboniferous succession of the Karakoram; conodonts (R. Mawson in Gaetani et al. 2008) date it to the Pragian. It underlies the peritidal Chilmarabad Formation and overlies the Ordovician Vidiakot slates.

Sources (3)

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: Defined in journal or other literature; not found in a GSP memoir. There is no body currently ratifying unit status, so provenance is shown in place of a formal ruling.

Cite this unit
APA

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

BibTeX
@misc{stratigraphypk_vandanilformation,
  author    = {Qudsi, Lareb},
  title     = {{Vandanil 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/vandanil-formation (accessed August 30, 2026).

To cite the unit's original definition instead, see: Gaetani et al. (2008).

    Saved on this device only.