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Pakistan Stratigraphy
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Mesozoic • Cretaceous

Sembar Formation

Early Cretaceous (Berriasian-Barremian)

Cretaceous in the time scale →

Stratigraphic position

In the Sulaiman Fold Belt column
Shale / mudSandstoneLimestoneFossils 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.

An Early Cretaceous black shale — the main source rock that generated the gas in Pakistan's Indus Basin fields.

Major source rock for hydrocarbons in Indus Basin. Deposited in anoxic marine conditions. Equivalent to Chichali in upper Indus.

Significance. An Early Cretaceous organic-rich marine shale that is the main petroleum source rock of the Indus Basin, deposited during Gondwana rifting as the Indian plate began to separate.

Lithology
Black, carbonaceous, pyritic shale with subordinate siltstone, sandstone and thin limestone; thins westward.
Thickness
100-300 m
Type locality
Sembar Pass, Sulaiman Range
Environment
marine, outer shelf
Economic importance
The principal hydrocarbon SOURCE ROCK of the Lower and Central Indus Basin (Sui, Mari and other gas fields); the Sembar–Lower Goru is an active petroleum system.

Fossils

AmmonitesBelemnitesForaminifera

References

Reviewer confidence: high

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