Shallow-marine, coastal-plain, and fluvial sediments of the Lower Permian Gharif Formation in the Interior Oman Sedimentary Basin presently range in depth from outcrop in the Huqf–Haushi area to almost 5000 m in the northwest. This large depth range results from a varied subsidence history with only minor uplift during the Late Triassic to Early Jurassic. The degree of diagenetic overprint varies, depending on burial history. Sandstone at shallow depth (,2600 m) shows intense dissolution of aluminosilicate and carbonate minerals, combined with minor kaolinite precipitation and compaction, whereas deeply buried sandstone (.2600 m) is highly compacted and tightly cemented by quartz, carbonate, and sulfate minerals. This varied diagenesis is caused by increasing temperature with burial, by surface-water infiltration during the Late Triassic to Early Jurassic, basin inversion and uplift in the Late Cretaceous along the southeastern basin margin, and obduction of the Oman Mountains in the Late Cretaceous. Depositional pore water was initially of low salinity (,50 g/l) with d18OSMOW values of 20.5 to 21.5‰ in the marine Lower Gharif and 2‰ in the arid Middle and Upper Gharif. During shallow burial (Late Triassic to Early Jurassic), pore water in the three Gharif members changed to high-salinity brines (;180 g/l) with d18OSMOW values of 24 to 27‰. Highly saline, deep-burial pore water with a heavy d18O signature (0.5–5‰) is the result of rock–water interactions in a rockdominated system. Present pore-water compositions mainly reflect subsurface dissolution of Ara Group evaporites, precipitation of late diagenetic carbonates and sulfates, and recharge of surface water along the uplifted southeastern basin margin

Shallow-marine, coastal-plain, and fluvial sediments of the Lower Permian Gharif Formation in the Interior Oman Sedimentary Basin presently range in depth from outcrop in the Huqf–Haushi area to almost 5000 m in the northwest. This large depth range results from a varied subsidence history with ...