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This outcrop analog study of Lower Khuff Sequence KS6 (Saiq Formation) aims to capture lateral reservoir facies distribution during the initial phase of basin-fill. The Hercynian tectonic event triggered the erosion of Cambrian to Carboniferous strata in Oman and formed the topography of the Sub-Khuff Unconformity. When the Neo-Tethys Ocean flooded the Arabian Shield clastic sediments, the so-called "Basal Khuff Clastics" became preferentially deposited in possible paleo-lows. One main objective of this study was to unravel the effect of this paleo-relief on reservoir facies distribution within the overlying sediments.

Khuff Sequence KS6: Paleorelief-influenced Facies and Sequence Patterns in the Lower Khuff Formation, Sultanate of Oman