By M. Younes
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Extra resources for Crude Oil Exploration in the World
When compared with effect of surface tension, this force becomes operational if there is a difference between the oil/air and oil/water interface tension, while it remains positive, the oil will spread out. Fay (1969), gave a theoretical treatment of the spreading of oils into three (3) separate phases. Where the spreading rate is controlled by the difference in density between the oil and the water and the speed of spreading controlled by inertia resistance. Where spreading rate is controlled by gravity but viscous drag between the oil and water limits the spreading rate.
Steckler, M. , 1985. Uplift and extension of the Gulf of Suez. Nature. 317, 135-139. Steckler, M. , F. Berthelot, N. Lyberris and Le Pichon, 1988. Subsidence in the Gulf of Suez: Implication for rifting and plate kinematics: Tectonophysics, 153, 249-270. K. and Moldowan, J. M. 1978. Applications of steranes, terpanes and monoaromatics to the maturation , migration and source of crude oils. Geochimica et Cosmochimica Acta, 42, 77-95. K. and Moldowan, J. M. 1981. Paleoreconstruction by biological markers.
1996. H. Freeman and company, New York. Khaled , K. A. 1999. Cretaceous source rocks at Abu Gharadig oil and gas field, North Western Desert, Egypt. Journal of Petroleum Geology, 22(24) pp. 377-395. McCain, W. 1998. Preparation of reservoir rock and fluid properties for simulation, Lower Bahariya Formation, Hayat-Yasser Field, Western Desert, Egypt. 406-421. M. Dahl, J. Huizinga, B. and Fago, F. 1994. The molecular fossil record of oleanane and its relation to angiosperms: Science, v. 768-771. Parker, J.
Crude Oil Exploration in the World by M. Younes