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Pakistan Stratigraphy
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Paleozoic • Ordovician–Silurian group

Baroghil group

Ordovician–Silurian

Karakoram-Hindukush Basin · Central Karakoram Batholith

Ordovician–Silurian in the time scale →

Stratigraphic position

In the Hindukush-Chitral column
MetamorphicSandstoneMixedShale / 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.

An Ordovician–Silurian sequence (the Yarkhun and Vidiakot formations) above the Ishkarwaz Granite at Baroghil Pass.

Baroghil group was named by Tahirkheli (1982) after the Baroghil pass, exposed in the Yarkhun valley, and south of Baroghil pass in Chitral district. Talent et al. (1999) have divided it into lower Yarkhun formation and upper Vidiakot formation.

Significance. The lower Paleozoic platform sequence (Ordovician–Silurian) that unconformably overlies the pre-Ordovician Ishkarwaz Granite south of the Baroghil Pass; it is divided into the lower Yarkhun Formation and the upper Vidiakot Formation (Talent et al., 1999) and carries Early Ordovician acritarchs and Middle–Late Ordovician conodonts. It is overlain with angular unconformity by the Devonian Chilmarabad Formation.

Lithology
Basal chert-rich conglomerate and arkosic sandstone with brachiopods, overlain by slate with metadolomite and quartzite.
Type locality
Baroghil Pass, Yarkhun valley, Chitral district
Basin
Karakoram-Hindukush Basin
Region
Central Karakoram Batholith
Environment
marine
Introduced by
Tahirkheli (1982)

Fossils

acritarchsconodontsbrachiopods

References

Reviewer confidence: medium

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