Abstract
Core samples of sandstone and clay raised from the Neogene succession of Sidi Salim-1 well were petrographically, mineralogically, and geochemically studied with the objective of determining the depositional conditions.
The sandstone is composed of quartz, feldspars of which the deeper sands of Qawasim Formation show some alteration; with rock fragments of volcanic, metamorphic, and sedimentary origin, in addition to altered biotite. These components are embedded in amorphous pyrite, microcrystalline calcite, and primary dolomite, as well as partial cementation by gypsum (mainly in the Pliocene sands).
The clays are composed primarily of montmorillonite, kaolinite, and illite. These clays were provided from mafic igneous rocks, sedimentary rocks, and intermediate igneous rocks, and were deposited under reducing conditions in a brackish lagoon intermittently receiving varying amounts of fresh water.