Shagai Limestone
Silurian(?)–Early Devonian
Northern Indus Suture
Silurian–Devonian in the time scale →Cited in 6 sources Last reviewed Jul 31, 2026
- Rank
- formation
- Status
- Under review
- Age
- Paleozoic · Silurian–Devonian · Silurian(?)–Early DevonianSilurian(?)–Early Devonian
- Named by
- Stauffer (1968)
- Type locality
- 1 km northeast of Shagai, Khyber Pass34.0172°N, 71.2800°E
- Thickness
- up to ~33 m
- Lithology
- Grey to black, partly brown limestone, thin- to thick-bedded, locally dolomitic and highly fractured, with thinly laminated limestone and sheared shale at the top.
- Synonyms
- Not recorded
A grey-to-black Silurian–Early Devonian limestone of the Khyber Pass, below the Ali Masjid Formation.
Fossils
Not recorded
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
- Northern Indus Suture
- Region
- Not recorded
- Depositional environment
- marine
- Coordinates
- 34.0172°N, 71.2800°E
Correlation
Not recorded. Compare this unit against other basins on the correlation panel →
Economic significance
Not recorded
Remarks
A largely unfossiliferous limestone of the Khyber Agency, exposed between the eastern Khyber Pass, Shagai Fort and Ali Masjid and in tectonic contact with the Khyber carbonate complex; its conformable contact beneath the Late Devonian Ali Masjid Formation makes it Silurian(?) to Early Devonian.
Sources (6)
- 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.
- Molloy, P.D., Talent, J.A. & Mawson, R. (1997). Late Devonian-Tournaisian conodonts from the eastern Khyber region, north-west Pakistan. Rivista Italiana di Paleontologia e Stratigrafia, 103(2), 123-148.
- 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.
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). Shagai Limestone. In Pakistan Stratigraphy Dataset [Data set]. Zenodo. https://doi.org/10.5281/zenodo.21363991
@misc{stratigraphypk_shagaiformation,
author = {Qudsi, Lareb},
title = {{Shagai Limestone} --- 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/shagai-formation (accessed September 5, 2026).
To cite the unit's original definition instead, see: Stauffer (1968).
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