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Pakistan Stratigraphy
Mesozoic Period

The Triassic in Pakistan

252 – 201 Ma

From 252 to 201 million years ago — life recovering from the greatest of all mass extinctions, with the supercontinent Pangaea at its height.

In Pakistan

The Triassic opens with the Mianwali Formation’s celebrated ceratite beds — ammonoids recording the recovery after the end-Permian extinction — and continues through the Tredian and Kingriali formations of the Salt Range and Trans-Indus ranges. Marine Triassic is also developed in Chitral and the Karakoram.

This reference records 33 units assigned to the Triassic across 6 basins, most commonly limestone, metamorphic rocks, sandstone.

At a glance

33
units
6
basins
11
provinces
7
georeferenced
15
with fossils
24
type localities
4,000 m
max thickness
30
sources

Rock types

  • limestone (18)
  • metamorphic rocks (7)
  • sandstone (3)
  • igneous rocks (2)
  • conglomerate (1)

Based on the primary lithology recorded for each unit; some units span more than one rock type.

Fossils recorded

  • Foraminifera
  • Algae
  • Megalodontidae (bivalves)
  • Benthic foraminifera (Aulotortus friedli, Agathammina)
  • Fusulinid foraminifera (Nankinella, Sphaerulina)
  • Dasyclad alga (Permocalculus)
  • Tubiphytes
  • Conodonts
  • Neospathodus dieneri
  • Triassospathodus homeri
  • Conodonts (Neospathodus homeri)
  • Meandrospira pusilla
  • megalodontid bivalves (Triassic)
  • colonial scleractinian corals (Triassic)
  • Parafusulina sp. (Permian base)
  • Megalodont bivalves
  • Gastropods
  • Claraia bivalves
  • Ophiceras ammonoids
  • Fish remains
  • Gyronites
  • Ambites
  • Proptychites
  • Koninckites

+13 more across the Triassic units.

Units of the Triassic

Provinces — Hazara Basin · Hindukush-Chitral · Karakoram · Khyber–Nowshera Belt · Kirthar Range · Kohat Basin · Potwar Basin · Salt Range · Sulaiman Fold Belt · Swat–Malakand · Zhob-Muslim Bagh.