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Pakistan Stratigraphy
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Paleozoic Literature

Chitral Slate

Late Palaeozoic

Cited in 3 sources Last reviewed Aug 29, 2026

Unit summary
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

In the Hindukush-Chitral column
LimestoneMetamorphicFossils recordedContact not recorded

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)

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)

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.

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Cite this unit
APA

Qudsi, L. (2026). Chitral Slate. In Pakistan Stratigraphy Dataset [Data set]. Zenodo. https://doi.org/10.5281/zenodo.21363991

BibTeX
@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).

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