- Rank
- Not recorded
- Status
- Published
- Age
- PaleozoicLate Palaeozoic
- Named by
- Not recorded
- Type locality
- Chitral region, northern Pakistan.
- Thickness
- Not recorded
- Lithology
- Fine-grained black slates with subordinate dark grey phyllite, quartzite and layers of limestone or marble; limestone dark grey to black, medium-grained, recrystallised.
- Synonyms
- Chitral Slates
The Chitral Slate is a Palaeozoic (largely Late Palaeozoic) slate-dominated succession of the Chitral region, correlated with the Darkot Group of the Gilgit area (Stauffer, 1975). It consists mainly of fine-grained black slates with subordinate phyllite, quartzite and limestone/marble intercalations.
Fossils
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
- Not recorded
- Region
- Not recorded
- Depositional environment
- Not recorded
- Coordinates
- Not recorded
Correlation
Not recorded. Compare this unit against other basins on the correlation panel →
Economic significance
Antimony: stibnite in quartz veins historically mined about 3 miles southwest of Partsan over a belt roughly 2 miles long, with further antimony mineralization reported northeast of Partsan in the Mastuj Valley (Heron 1950; Stauffer 1975).
Remarks
Not recorded
Research notes (4)
Field-by-field findings drawn from the cited literature. Every statement is traced to a registered source — follow a citation for the full reference.
Lithology (2)
-
Mujtaba et al. (2024): the Chitral Slates are fine-grained black slates with subordinate dark grey phyllite, quartzite and limestone/marble layers (dark grey-black, medium-grained, recrystallised); Palaeozoic (likely Late Palaeozoic), correlated with the Darkot Group of the Gilgit Agency (Stauffer 1975).
-
Upper Palaeozoic schists and (meta-)volcanics of the Chitral area (Chitral Slates), part of the geosynclinal succession of the Central Hindu Kush (Buchroithner & Gamerith 1986).
Fossils & biostratigraphy (1)
-
Stauffer (1975): the only fossils recovered from the Chitral Slate are a Spirifer, a small Dielasma and two unidentified corals, collected by Tipper (in Fermor 1922) from a calcareous layer within the slates in the Chitral Gol; on this sparse evidence the formation is dated only as Paleozoic, probably in part late Paleozoic.
Stauffer, K.W. (1975)
Economic significance (1)
-
Stauffer (1975, after Heron 1950): antimony sulfides occur in quartz veins in the Chitral Slate and have been mined in a ~2-mile-long belt about 3 miles SW of Partsan, with additional antimony showings NE of Partsan in the Mastuj Valley.
Stauffer, K.W. (1975)
Sources (1)
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: 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
Qudsi, L. (2026). Chitral Slate. In Pakistan Stratigraphy Dataset [Data set]. Zenodo. https://doi.org/10.5281/zenodo.21363991
@misc{stratigraphypk_chitralslate,
author = {Qudsi, Lareb},
title = {{Chitral Slate} --- 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/chitral-slate (accessed October 29, 2026).
Related units
Referenced in other successions
Overlain by Darkot Group
Underlain by Reshun Formation
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