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Here we present the stratigraphic architecture and carbonate platform evolution of the Middle Permian (Capitanian) succession (Wargal Formation) of Trans‐Indus Ranges, central Pakistan. The exposed carbonate sequence consists of thin‐ to thick‐bedded bioclastic, nodular, fine‐grained, and sandy limestone. Based on detailed petrographic studies, seven microfacies assemblages have been recognized, suggesting...
The present study integrates the facies and planktonic foraminiferal biostratigraphic data to construct a sequence stratigraphic model of the Mughal Kot Formation of Maastrichtian age in the Lower Indus Basin, Pakistan. The Mughal Kot Formation is comprised of 1000-m-thick sequence of hemipelagic sediments, interrupted by random influxes of coarse-grained sandy turbidites. The petrographic details...
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