Ganchen Formation
Devonian–Permian
Karakoram-Hindukush Basin · Southern Metamorphic Belt
Devonian–Permian in the time scale →Cited in 4 sources Last reviewed Jul 18, 2026
- Rank
- formation
- Status
- Published
- Age
- Paleozoic · Devonian–PermianDevonian–Permian
- Named by
- Desio (1963)
- Type locality
- Ganchen Peak (6462 m), north of the Shigar valley, Skardu district
- Thickness
- Not recorded
- Lithology
- Metapelite with less common gneiss and amphibolite and thick beds of crystalline limestone and dolomite; pelites carry a kyanite–staurolite–garnet–biotite–muscovite–plagioclase–quartz assemblage.
- Synonyms
- Not recorded
A high-grade metapelite-and-marble unit near Ganchen Peak, part of the Karakoram Metamorphic Complex.
Ganchen formation is named after the Ganchen peak (6462m) by Desio (1963) exposed in the Shigar valley (Skardu district) and consists of metapelites, gneisses, amphibolites, limestone and dolomite. Metamorphic grade is increasing NW and slates are converted into garnet biotite schists. Hanson (1989) named this sequence as Daltumbore formation while Desio (1963) included the Lugma slates, Daltumbore mica schist and Askore amphibolite in this sequence. The age is assigned from Devonian to Permian by Brookfield and Gupta (1984) and Hanson (1989).
Fossils
Not recorded
Contacts
Band colour = period; texture = dominant rock type. Lines between bands mark the contact type; dotted = no contact recorded in the sources (not a claim of conformity). 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
- Not recorded
- Coordinates
- Not recorded
Correlation
Not recorded. Compare this unit against other basins on the correlation panel →
Economic significance
Not recorded
Remarks
A metapelite–marble unit of the Karakoram Metamorphic Complex north of Shigar, in contact with the Dumordo Formation; assigned a Devonian to Permian age (Brookfield and Gupta, 1984; Hanson, 1989). Searle (1991) extended the name to include the Chalt Formation of Hunza.
Research notes (1)
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)
Sources (3)
- 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.
- 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). Ganchen Formation. In Pakistan Stratigraphy Dataset [Data set]. Zenodo. https://doi.org/10.5281/zenodo.21363991
@misc{stratigraphypk_ganchenformation,
author = {Qudsi, Lareb},
title = {{Ganchen 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/ganchen-formation (accessed October 29, 2026).
To cite the unit's original definition instead, see: Desio (1963).
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