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Pakistan Stratigraphy
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Precambrian • Neoproterozoic-Cambrian GSP memoir

Misgar Slate

Late Precambrian-Cambrian

Neoproterozoic-Cambrian in the time scale →

Cited in 7 sources Last reviewed Aug 20, 2026

Unit summary
Rank
Not recorded
Status
Published
Age
Precambrian · Neoproterozoic-CambrianLate Precambrian-Cambrian
Named by
Not recorded
Type locality
Misgar, Upper Hunza, Gilgit-Baltistan36.7875°N, 74.7682°E
Thickness
1500-2000 m
Lithology
Black slate, phyllite, quartzite
Synonyms
Not recorded

Black slates and phyllites of upper Hunza (Misgar area) representing deep-marine deposition on the southern edge of the Asian plate; its age is debated in the literature.

Exposed in Misgar area of upper Hunza. Low-grade metamorphic sequence representing deep marine conditions on the southern margin of the Asian plate.

Fossils

Not recorded

Contacts

In the Karakoram column
LimestoneMetamorphicConformableUnconformity

Band colour = period; texture = dominant rock type. Lines between bands mark the contact type (wavy = unconformity inferred from a missing period). 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
36.7875°N, 74.7682°E

Correlation

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

Economic significance

Not recorded

Remarks

A low-grade metamorphic slate-phyllite succession of the upper Hunza (Misgar) area, on the southern margin of the Asian (Karakoram) plate. Baseline age is Late Precambrian-Cambrian; note that some Karakoram literature instead assigns the Misgar Slate a much younger (Paleocene) age, so the age is regionally debated and left at the baseline value here.

Sources (6)
  • Malkani, M.S. & Mahmood, Z. (2017). Stratigraphy of Pakistan. Geological Survey of Pakistan, Memoir Vol. 24.
  • OpenStreetMap contributors and GEOnet Names Server (public geographic gazetteers), used to geolocate named GSP type localities to approximate decimal coordinates.
  • Kazmi, A.H. & Jan, M.Q. (1997). Geology and Tectonics of Pakistan. Graphic Publishers, Karachi.
  • Kazmi, A.H. & Abbasi, I.A. (2008). Stratigraphy and Historical Geology of Pakistan. Department & National Centre of Excellence in Geology, University of Peshawar, Peshawar. 524 pp. ISBN 978-969-9119.
  • Coward, M.P., Jan, M.Q., Rex, D., Tarney, J., Thirlwall, M. & Windley, B.F. (1984). Geology of the South Central Karakoram and Kohistan. In: Miller, K.J. (ed.), The International Karakoram Project, Vol. 2, 71-84. Cambridge University Press.
  • Tahirkheli, R.A.K., Sun Dongli, Pan Yushang, Deng Wanming, Zhang Yuquan, Baqri, S.R.H. & Dawood, H. (1990). Review of stratigraphy of the Upper Hunza Valley (UHV), NW Karakoram, Pakistan. Geological Bulletin, University of Peshawar, 23, 203-214.

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: Appears in a single-author Geological Survey of Pakistan memoir (Malkani & Mahmood 2017), not cross-confirmed against the Shah lexicon. The Stratigraphic Committee of Pakistan is largely inactive, so documented provenance — not formal ratification — is the available signal.

Cite this unit
APA

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

BibTeX
@misc{stratigraphypk_misgarslate,
  author    = {Qudsi, Lareb},
  title     = {{Misgar 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/misgar-slate (accessed August 30, 2026).

    Saved on this device only.