By M. Younes

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A. 1998. Kenz Field: A new play concept in Khalda Concession. 118-138. Abdel-Gawad, E. , Philip, R. P. and Zein El-Din, M. Y. 1996. Evaluation of possible source rocks in Faghur-Siwa Basin, Western Desert, Egypt. Proceeding of the EGPC 13th Petroleum Exploration and Production Conference, Cairo. 1, pp. 417-432. , 1998. Deep wells in Khalda West: A brief review. 517-533. Al-Sharhan, A. S. and Abdel-Gawad, E. A. 2002. Integrating kerogen and bitumen analyses to enhance characterization of source rocks in northwestern Desert of Egypt.

The plotting of the stable carbon isotopic composition to the saturate and aromatic fractions of the studied crude oils in addition to the source rock extracts are shown in (Figure 12). 6 ‰PDB. 5 ‰PDB. The figure reveals that the studied crude oils are of terrestrial origin and the organic matter responsible for hydrocarbon generation in shale source rock of Khatatba, Alam El-Bueib and Hydrocarbon Potentials in the Northern Western Desert of Egypt 43 Abu Roash-G were probably originated from terrestrial sources.

The Geology of Egypt: Amesterdam, Elsevier, 317p. 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.

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