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Pakistan Stratigraphy
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Mesozoic • Jurassic-Cretaceous

Chichali Formation

Late Jurassic - Early Cretaceous

Jurassic-Cretaceous in the time scale →

Stratigraphic position

In the Salt Range column
SandstoneLimestoneShale / mudFossils 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.

A greenish, glauconite-rich marine sandstone and shale marking the Jurassic-to-Cretaceous transition in the Upper Indus Basin.

Named after Chichali Pass in Surghar Range. Marks Jurassic-Cretaceous boundary. Rich in belemnites. Correlated with Spiti Shale of Hazara. Part of the Chichali Group.

Significance. A glauconitic marine sandstone-and-shale unit straddling the Jurassic–Cretaceous boundary in the Kohat–Potwar region; its glauconite and condensed character record slow marine sedimentation, and it underlies the Cretaceous Lumshiwal Formation.

Lithology
Dark greenish grey glauconitic sandstone, glauconitic shale
Type locality
Chichali Pass in Surghar
Environment
marine
Introduced by
Danilchik (1961)
Economic importance
Phosphorite (rock phosphate) has been reported from the Chichali Formation near Kohat, but low phosphate content makes it of little economic value.

References

Reviewer confidence: medium

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