Gum Formation
Permian–Cretaceous
Karakoram-Hindukush Basin · Southern Metamorphic Belt
Permian in the time scale →Cited in 4 sources Last reviewed Jul 30, 2026
- Rank
- formation
- Status
- Published
- Age
- Paleozoic · PermianPermian–Cretaceous
- Named by
- Le Fort & Gaetani (1998)
- Type locality
- Qalandar Gum glacier, upper Yasin/Darkot region
- Thickness
- about 1000 m
- Lithology
- About 1000 m of limestone and slate.
- Synonyms
- Not recorded
A thick (about 1000 m) Permian limestone-and-slate unit of the Darkot Group.
Gum formation (1000m) is named after Qalandar Gum glacier and consists of limestone and slates. Gaetani (2004) mentioned the Permian to Triassic or up to Cretaceous.
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
- Karakoram-Hindukush Basin
- Region
- Southern Metamorphic Belt
- Depositional environment
- marine
- Coordinates
- Not recorded
Correlation
Not recorded. Compare this unit against other basins on the correlation panel →
Economic significance
Not recorded
Remarks
A thick limestone-and-slate unit of the Darkot Group (its Southern Stack); assigned a Permian age, though Gaetani (2004) suggested it may range up into the Triassic or even the Cretaceous.
Research notes (3)
Field-by-field findings drawn from the cited literature. Every statement is traced to a registered source — follow a citation for the full reference.
Name & nomenclature (1)
-
Attested in Shah (2009), Geological Survey of Pakistan Memoir 22 - the Stratigraphic Committee of Pakistan's compiled lexicon (listed in the memoir's contents). Adds the definitional GSP/SCP lexicon citation.
Shah, S.M.I. (2009)
Age & correlation (1)
-
Zanchi & Gaetani (2011): the Gum Formation (Le Fort & Gaetani 1998; Darkot Group) is Permian to Triassic — Member 1 carries a Permian-aspect bryozoan/brachiopod fauna, Member 2 Late Triassic megalodontids. Well-bedded recrystallized limestones and dolostones (Mb 2 >700 m; Mb 1 ≥300 m). NB: the curated top age 'Cretaceous' is not supported by this paper (Triassic top) — flagged for reconciliation.
Lithology (1)
-
CONFIRMED against Zanchi & Gaetani (2011, full text): massive light limestone/dolostone (named after the Qalandar Gum Glacier) with a Permian-aspect bryozoan-brachiopod fauna. Supports a Permian age; the Cretaceous extension in the dataset is NOT confirmed by this map.
Sources (3)
- Malkani, M.S. & Mahmood, Z. (2017). Stratigraphy of Pakistan. Geological Survey of Pakistan, Memoir Vol. 24.
- Zanchi, A. & Gaetani, M. (2011). The geology of the Karakoram range, Pakistan: the new 1:100,000 geological map of Central-Western Karakoram. Italian Journal of Geosciences, 130(2), 161-262.
- Shah, S.M.I. (2009). Stratigraphy of Pakistan. Geological Survey of Pakistan, Memoir Vol. 22.
Reviewer confidence: medium
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). Gum Formation. In Pakistan Stratigraphy Dataset [Data set]. Zenodo. https://doi.org/10.5281/zenodo.21363991
@misc{stratigraphypk_gumformation,
author = {Qudsi, Lareb},
title = {{Gum 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/gum-formation (accessed October 7, 2026).
To cite the unit's original definition instead, see: Le Fort & Gaetani (1998).
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