The Middle Jurassic was a time of marginal to shallow shelf settings dominated by organic matter-rich deposition in northern Egypt, southern Tethys. Paleoenvironmental and sequence stratigraphic reconstructions are paramount significance for better understanding basin history related reservoirs source rock units. For this purpose, detailed palynomorph palynofacies analysis the Khatatba Formatio...

The most prolific reservoir intervals in the Barents Sea are found Upper Triassic to Middle Jurassic Realgrunnen Subgroup, deposited during a major change structural evolution of basin which greatly influenced its development and distribution. effects evident one petroleum provinces SW Sea, Hoop Area. Due condensed nature succession, tectonostratigraphic has been enigmatic. We use range differe...

The Middle Jurassic in the north Western Desert, Egypt, was a time of complex tectonics and increased environmental perturbations attributed to predominant sedimentation organic carbon-rich fine siliciclastic carbonate deposits Khatatba Formation. Although some studies have addressed hydrocarbon potential source rock characteristics Formation, regional-scale investigation prevalent paleoenviron...