Abstract:The Late Permian succession of the Upper Indus Basin in northeastern Pakistan is represented by the carbonate‐dominated Zaluch Group, which consists of the Amb, Wargal and Chhidru formations, which accumulated on the southwestern shelf of the Paleo‐Tethys Ocean, north of the hydrocarbon‐producing Permian strata of the Arabian Peninsula. The reservoir properties of the mixed clastic‐carbonate Chhidru Formation (CFm) are evaluated based on petrography, using scanning electron microscopy (SEM), energy dispersive … Show more
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