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Paleozoic group Redefined In GSP lexicon

Alpurai Group

Paleozoic–Mesozoic

Northern Indus Suture · Malakand

Cited in 8 sources Last reviewed Aug 10, 2026

Unit summary
Rank
group
Status
Published
Age
PaleozoicPaleozoic–Mesozoic
Named by
DiPietro (1990)
Type locality
Alpurai, Swat34.9000°N, 72.6500°E
Thickness
Not recorded
Lithology
Unfossiliferous siliceous schist, calcareous quartz-mica-garnet schist, marble and para-amphibolite.
Synonyms
Not recorded
Nomenclature

Redefined. First defined by DiPietro (1990).

Browse all alternative & superseded names →

The Paleozoic–Mesozoic schist-and-marble cover of the Swat Nappe — the Marghazar, Kashala, Saidu and Nikanai Ghar formations.

Alpurai group is renamed by DiPietro (1990) after the Alpurai schist of Kazmi et al. (1984). Di Pietro (1990) mentioned the Marghazar, Kashala, Nakanai Ghar and Saidu formations in this group. 31

Fossils

Not recorded

Contacts

In the Swat–Malakand column
MixedMetamorphicLimestoneContact not recordedUnconformity

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.

Constituent units

Formations that make up this group, in stratigraphic order (youngest at top, as in the column).

  1. 1 Saidu Formation Triassic–Jurassic
  2. 2 Nikanai Ghar Formation Triassic
  3. 3 Kashala Formation Triassic
  4. 4 Marghazar Formation Carboniferous

Distribution & setting

Basin
Northern Indus Suture
Region
Malakand
Depositional environment
Not recorded
Coordinates
34.9000°N, 72.6500°E

Correlation

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

Economic significance

Not recorded

Remarks

The Paleozoic–Mesozoic metasedimentary cover of the Precambrian Manglaur Schist (Swat Nappe), resting unconformably on the Swat Granite Gneiss; originally the 'Alpurai Schists' (Kazmi et al., 1984c), redefined by DiPietro (1990) to include the Marghazar, Kashala, Saidu and Nikanai Ghar formations.

Research notes (5)

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 (2)

  • 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)

  • DiPietro et al. (1993): introduced by Kazmi et al. (1984) as the 'Alpurai schist' and raised to group rank — subdivided into the Marghazar, Kashala, Saidu and Nikanai Ghar formations — by DiPietro (1990). The group records Late-Palaeozoic breakup of Gondwana, a passive Mesozoic shelf, and drowning of the shelf at the onset of the Himalayan orogeny; it unconformably overlies the Manglaur Formation and the Swat granitic gneiss.

    DiPietro, J.A., Pogue, K.R., Lawrence, R.D., Baig, M.S., Hussain, A. & Ahmad, I. (1993)

Age & correlation (1)

  • DEFINED by DiPietro et al. (1993, full text): the Alpurai Group (Lower Swat, south of the Main Mantle Thrust) = Marghazar Formation (Carboniferous or younger) + Kashala, Saidu and Nikanai Ghar formations (Triassic or younger); it unconformably overlies the Manglaur formation, with the Jobra formation in lenses beneath. Type sections designated for each unit. This is the defining paper for the group.

    DiPietro, J.A., Pogue, K.R., Lawrence, R.D., Baig, M.S., Hussain, A. & Ahmad, I. (1993)

Geological significance (2)

  • The Alpurai Group metasediments record a south-to-north increasing Barrovian metamorphic gradient (Ahmad, Jan & Jehan 2005): greenschist facies (biotite grade; ~300-400 C, <=3 kb) around Takht-e-Bhai and Rustam in the south, rising to epidote-amphibolite facies (garnet-kyanite grade; ~580 C, ~5.5 kb) near Mora Kandao / Malakand in the north.

    Ahmad, I., Jan, M.Q. & Jehan, N. (2005)

  • Anczkiewicz et al. (1998): the Alpurai Schists/Group (mica-garnet calc-schists) reach amphibolite facies up to kyanite grade (minimum ~550 C at 7 kbar) - not the greenschist grade of earlier work; their lower-part metabasalts likely represent the Permian Panjal Trap (Gondwana-break-up rifting). 40Ar-39Ar amphibole ages bracket the onset of post-collisional normal faulting on the Indus Suture at ~37-40 Ma.

    Anczkiewicz, R., Burg, J.-P., Hussain, S.S., Dawood, H., Ghazanfar, M. & Chaudhry, M.N. (1998)

Sources (8)

Reviewer confidence: high

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.

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Cite this unit
APA

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

BibTeX
@misc{stratigraphypk_alpuraigroup,
  author    = {Qudsi, Lareb},
  title     = {{Alpurai Group} --- 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/alpurai-group (accessed October 29, 2026).

To cite the unit's original definition instead, see: DiPietro (1990).

    Saved on this device only.