Skip to content
Pakistan Stratigraphy
Suggest a correction
Mesozoic • Cretaceous–Paleogene group

Dir group

Cretaceous–Paleocene

Kohistan-Ladakh Magmatic Arc · Northern Greenstone Belt

Cretaceous–Paleogene in the time scale →

Stratigraphic position

In the Kohistan Arc column
MetamorphicShale / mudConformable

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.

The Dir Group — the Baraul Banda slate and Utror volcanics — the latest-Cretaceous–Paleocene record of Kohistan-arc volcanism.

Dir group ( Latest Cretaceous-Paleocene) named by Tahirkheli (1979) which include the Baraul Banda slate and Ultor volcanic formation. Baraul Banda slate contains shale, wakes, calcareous beds and some volcanics.

Significance. The latest-Cretaceous–Paleocene arc succession of the Dir–Chitral region, comprising the Baraul Banda slate and the Utror volcanics; records the youngest, waning phase of Kohistan-arc volcanism before final collision.

Lithology
Baraul Banda slate (shale, greywacke, calcareous beds and volcanics) and the Utror volcanic formation.
Basin
Kohistan-Ladakh Magmatic Arc
Region
Northern Greenstone Belt
Environment
volcanic-arc, marine
Introduced by
Tahirkheli (1979)

Provinces

References

  • Malkani, M.S. & Mahmood, Z. (2017). Stratigraphy of Pakistan. Geological Survey of Pakistan, Memoir Vol. 24.
  • Kazmi, A.H. & Jan, M.Q. (1997). Geology and Tectonics of Pakistan. Graphic Publishers, Karachi.

Reviewer confidence: high

    Saved on this device only.