Kundil Formation
Permian
Karakoram-Hindukush Basin · Central Karakoram Batholith
Permian in the time scale →Cited in 8 sources Last reviewed Aug 20, 2026
- Rank
- formation
- Status
- Published
- Age
- Paleozoic · Permian · Late PermianPermian
- Named by
- Gaetani et al. (1990a)
- Type locality
- Kundil valley36.7100°N, 74.7700°E
- Thickness
- cherty limestone about 100–120 m (Wirokhun Saddle / Borom gullies west of Sost), with a laterally thinning megabreccia body in the middle–upper part
- Lithology
- Cherty limestone with marl and fine tuff: a lower thick-bedded cherty limestone unit, a middle grey cherty limestone unit, and an upper unit, with a metabreccia up to 100 m thick between the middle and upper units.
- Synonyms
- Not recorded
The Late Permian cherty-limestone top of the Chapursan Group in upper Hunza.
Kundil formation is named after Kundil valley, south of Darband post about 10km NW of Sost (Shimshal and Chapursan Valleys of upper Hunza) by Gaetani et al. (1990a), presented 3 members of marl, limestone and fine tuffs of Late Permian age.
Fossils
Contacts
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
- Coordinates
- 36.7100°N, 74.7700°E
See it in the field
Geoheritage site where this unit is exposed at outcrop.
Correlation
Not recorded. Compare this unit against other basins on the correlation panel →
Economic significance
Not recorded
Remarks
Uppermost Permian formation of the Chapursan Group in the Upper Hunza region; conformably overlies the Panjshah Formation.
Sources (7)
- Malkani, M.S. & Mahmood, Z. (2017). Stratigraphy of Pakistan. Geological Survey of Pakistan, Memoir Vol. 24.
- Kazmi, A.H. & Jan, M.Q. (1997). Geology and Tectonics of Pakistan. Graphic Publishers, Karachi.
- OpenStreetMap contributors and GEOnet Names Server (public geographic gazetteers), used to geolocate named GSP type localities to approximate decimal coordinates.
- Shah, S.M.I. (2009). Stratigraphy of Pakistan. Geological Survey of Pakistan, Memoir Vol. 22.
- Gaetani, M., Nicora, A., Henderson, C., Cirilli, S., Gale, L., Rettori, R., Vuolo, I. & Atudorei, V. (2013). Refinements in the Upper Permian to Lower Jurassic stratigraphy of Karakorum, Pakistan. Facies, 59, 915-948.
- Kazmi, A.H. & Abbasi, I.A. (2008). Stratigraphy and Historical Geology of Pakistan. Department & National Centre of Excellence in Geology, University of Peshawar, Peshawar. 524 pp. ISBN 978-969-9119.
- Gaetani, M., Angiolini, L., Garzanti, E., Jadoul, F., Leven, E.Ya., Nicora, A. & Sciunnach, D. (1995). Permian stratigraphy in the Northern Karakorum, Pakistan. Rivista Italiana di Paleontologia e Stratigrafia, 101(2), 107-152.
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
Qudsi, L. (2026). Kundil Formation. In Pakistan Stratigraphy Dataset [Data set]. Zenodo. https://doi.org/10.5281/zenodo.21363991
@misc{stratigraphypk_kundilformation,
author = {Qudsi, Lareb},
title = {{Kundil 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/kundil-formation (accessed September 5, 2026).
To cite the unit's original definition instead, see: Gaetani et al. (1990a).
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