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Paleozoic • Silurian–Devonian formation Literature

Daradar Dolomite

Silurian to Devonian (correlation)

NW Indian plate margin · Spinghar (Safed Koh) Range

Silurian–Devonian in the time scale →

Cited in 1 source Last reviewed Aug 2, 2026

Unit summary
Rank
formation
Status
Published
Age
Paleozoic · Silurian–DevonianSilurian to Devonian (correlation)
Named by
Badshah et al. (2000)
Type locality
Spinghar (Safed Koh) Range, NW Pakistan–SE Afghanistan border region.
Thickness
Not recorded
Lithology
Siliceous, white to greyish-white, hard dolomite (up to ~19 wt% MgO) with dolerite intrusions; talc/soapstone along fractures and intrusive contacts.
Synonyms
Not recorded

A Siluro-Devonian siliceous dolomite of the Spinghar (Safed Koh) Range on the NW Indian-plate margin, introduced by Badshah et al. (2000). White to greyish-white and hard, it overlies the Spinghar Crystalline unit, is cut by dolerite intrusions, and carries talc (soapstone) and silver-rich lead-copper mineralisation along fracture zones. It is correlated with Silurian-Devonian rocks of the Khyber Agency.

Fossils

Not recorded

Contacts

In the Khyber–Nowshera Belt 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
NW Indian plate margin
Region
Spinghar (Safed Koh) Range
Depositional environment
shallow marine
Coordinates
Not recorded

Correlation

Not recorded. Compare this unit against other basins on the correlation panel →

Economic significance

Hosts talc (soapstone) along fracture zones and mafic-intrusion contacts, and silver-rich lead-copper mineralisation in the western Spinghar (Neemtota).

Remarks

Overlies the Spinghar Crystalline basement and is disconformably(?) overlain by the Spinghar Quartzite; forms south-facing cliffs in the Spinghar nappe (Badshah et al. 2000).

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.

Geological significance (1)

  • One of six lithostratigraphic units defined for the Spinghar / South Waziristan area (with Spinghar Quartzite, Sikaram Series, Makai Limestone, Wana Schist and Kaniguram Slate) in the tectonostratigraphic framework of the NW Indian plate and Kabul block (Badshah et al. 2000).

    Badshah, M.S., Gnos, E., Jan, M.Q. & Afridi, M.I. (2000)

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). Daradar Dolomite. In Pakistan Stratigraphy Dataset [Data set]. Zenodo. https://doi.org/10.5281/zenodo.21363991

BibTeX
@misc{stratigraphypk_daradardolomite,
  author    = {Qudsi, Lareb},
  title     = {{Daradar Dolomite} --- 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/daradar-dolomite (accessed October 29, 2026).

To cite the unit's original definition instead, see: Badshah et al. (2000).

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