Indo-Pakistan Shield (Precambrian Craton)
Indo-Pakistan Shield
Scattered exposures: Sargodha-Chiniot (Punjab), Nagarparkar (Sindh), Besham-Swat (KP), Nanga Parbat (GB) · Stable cratonic shield with scattered inselberg exposures and Himalayan tectonic windows
Precambrian crystalline basement of the Indian Plate exposed as inselbergs in Punjab-Sindh plains (Kirana Hills, Nagarparkar) and in the Lesser Himalayan nappes (Besham, Swat). Includes Archean to Neoproterozoic gneisses, granites, volcanics, and metamorphic complexes. Records the oldest geological history of Pakistan (>2.5 Ga).
Units
20
Tectonic setting
Stable cratonic shield with scattered inselberg exposures and Himalayan tectonic windows
This reference records 20 units in the Indo-Pakistan Shield spanning 1 geological era, most commonly metamorphic rocks, conglomerate, igneous rocks.
At a glance
- 20
- units
- 1
- era
- 10
- georeferenced
- 0
- with fossils
- 14
- type localities
- 3,000 m
- max thickness
- 10
- sources
Rock types
- metamorphic rocks (11)
- conglomerate (5)
- igneous rocks (2)
- evaporite (2)
Based on the primary lithology recorded for each unit; some units span more than one rock type.
Units in this province
20 unitsLine these up against other basins on the correlation panel →
- Quaternary
- Cenozoic
- Mesozoic
- Paleozoic
- Precambrian
Which part?
- Chiniot Granite
- Hachi Volcanic Group
- Kirana Group
- Nagarparkar Igneous Complex
- Sharaban Group
- Taguwali Formation
- Nanga Parbat Gneiss
- Petaro-Hyderabad Ridge
- Asianwala Formation
- Buland Hill Formation
- Chak 102 Conglomerate
- Chak 112 Conglomerates
- Hadda Quartzite
- Machh Super Group
- Wad Sayyidan Formation
- Iskere Gneiss
- Mangla Gneiss
- Shingus Gneiss
- Sargodha Ridge Basement
- Besham Group
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.