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Pakistan Stratigraphy
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Mesozoic • Cretaceous–Paleogene formation In GSP lexicon

Bauma Harel Formation

Cretaceous–Eocene (uncertain; ?Jurassic)

Karakoram-Hindukush Basin · Central Karakoram Batholith

Cretaceous–Paleogene in the time scale →

Cited in 5 sources Last reviewed Aug 2, 2026

Unit summary
Rank
formation
Status
Published
Age
Mesozoic · Cretaceous–PaleogeneCretaceous–Eocene (uncertain; ?Jurassic)
Named by
Kazmi and Abbasi (2008)
Type locality
Bauma Harel locality, Askole–Skoro Lungma and Thalle area, northeast of Skardu
Thickness
Not recorded
Lithology
Volcanic metasediments metamorphosed to chlorite–epidote greenschist, interbedded with slate, phyllite, minor carbonate layers and conglomerate; the lower part comprises amphibolite, marble and metapelite basement.
Synonyms
Not recorded

Ancient (Late Proterozoic) crystalline basement near Skardu, capped by an Early Ordovician fossil-bearing cover.

Bauma Harel formation is named after the Bauma Harel locality by Kazmi and Abbasi (2008) for the sequence of amphibolites, marbles and metapelites bear a minimum Ar-Ar age of 650Ma, in the Askole-Skoro Lungma, Bauma Harel and Thalle village areas in the NE of Skardu. These rocks form the Late Proterozoic basements and also in the Baroghil area of western Karakoram, they are overlain by platform type sedimentary sequence with lower Ordovician fossils (crinoids and graptolites). Bauma-Harel formation consists of volcanic metasediments metamorphosed to chloriteepidote greenschists interbedded with slate, phyllite, minor carbonate layers and conglomerate.

Fossils

turritellid gastropods

Contacts

In the Karakoram column
IgneousConglomerateMetamorphicFossils recordedConformable

Band colour = period; texture = dominant rock type. Lines between bands mark the contact type. 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
Central Karakoram Batholith
Depositional environment
volcanic
Coordinates
Not recorded

Correlation

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

Economic significance

Not recorded

Remarks

A Late Proterozoic crystalline basement (amphibolite, marble and metapelite with a minimum Ar–Ar age of about 650 Ma) overlain by a platform sequence that carries Early Ordovician crinoids and graptolites; recognised in the western Karakoram and the Baroghil area.

Sources (5)

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
APA

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

BibTeX
@misc{stratigraphypk_baumaharelformation,
  author    = {Qudsi, Lareb},
  title     = {{Bauma Harel 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/bauma-harel-formation (accessed August 30, 2026).

To cite the unit's original definition instead, see: Kazmi and Abbasi (2008).

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