The idea is to create a 3D grid and layer this grid. Then sample the interval velocity (derived after Dix conversion of the stacking velocity) into this simple grid (up scaling). The last step is to populate the interval velocity as a property into the grid through Kriging. Pseudo-velocity 2-D ModelingContinue Reading

Abstract The Nile, Nile Delta Regional Framework and the Mediterranean Sea, their tectonics and Their Geological history are considered the basis for understanding the exploration plays and consequently the upside potentials for hydrocarbons in the Nile Delta. Through regional mapping of Cretaceous, Oligocene, Miocene and Pliocene, at both onshore and offshore Nile Delta, many lessons...Continue Reading