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A. and Posthuma, J. 1974. On the origin of sulfur in crude. 1973, eds. B. Tissot and F. Bienner, 727-739. , 1992. 18-19. Hunt, J. , 1996. Petroleum Geochemistry and Geology: New York, Freeman, 743 p. Isaksen, G. H. 2004, Central North Sea hydrocarbon systems: Generation, migration, entrapment and thermal degradation of oil and gas. American Association of Petroleum Geologist Bulletin, 68, 1545-1572. Khalil, M. and Moustafa, A. 1995. Tectonic framework of northeast Egypt and its bearing on hydrocarbon exploration.
1974). Figure (4) shows a plot of hydrogen index (HI) versus oxygen index (OI) on Van Krevelen diagram for the studied shale source rock intervals of Khatatba, Alam El-Bueib and Abu Roash-G from well Shushan-1X. The figure shows that Khatatba Alam El-Bueib and Abu Roash shales contain mixed kerogen types II-III. ,1994). Mixed kerogen type characterizes mixed environment containing admixture of continental and marginal marine organic matter have the ability to generate oil and gas accumulations (Hunt, 1996).
1986. Biomarker distributions in oils predominantly derived from terrigenous source materials. In advances in Organic Geochemistry 1985, eds. D. Leythaeuser and R. Rullkőtter. Organic Geochemistry 10, 73-84, Pergamon, Oxford. , Littke, R. and Rullkőtter, J. 1997. Maturation and petroleum generation. In migration of hydrocarbons in sedimentary basins, ed. B. Doligez. 649-665. G. 1982. Crude oil geochemistry of the Gulf of Suez. 6th EGPC Exploration and Production Conference, v. 1, p. 212-224. Said, R.