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Trace metals such as arsenic (AS) decreases hydrogenation and isomerisation activity of catalysts, acting as permanent poison (Hettinger et al, 1955). Gas and coke formation in crack stock is enhanced by copper (Cu) which promotes low gasoline production. Iron (fe) poisons catalysts and accelerates oxidation, which may result in unstable products (Milner, 1963, Ming and Bott 1956, Karchmer and Gunn 1952), Nickel deposits contaminate cracking catalysts more than any common metal leading to low gasoline yield.

E. and Fowler, M. G. 2002, Application of petroleum geochemistry to exploration and reservoir management. Organic Geochemistry, v. 33, pp. 5-36. Shahin, A. N. and Lebbudy, M. M. 2002. Geohistory analysis, mapping of source beds, timming of hydrocarbon generated and undiscovered reserves in East Abu Gharadig Basin, Western Desert, Egypt. AAPG International Petroleum Conference and Exhibition, Cairo. Accepted Abstract. N. ,1988. Undiscovered hydrocarbon reserves and their preservation time basin, Western Desert, Egypt.

El-Ghamri , M. A. and Mostafa, A. R. 2004. Geochemical evaluation of the possible source rocks in the October Field, Gulf of Suez, Egypt. Sedimentological Society of Egypt, v. 12, p. 55-67. Ekweozor, C. , Okogun, J. U. and Maxwell, J. R. 1979. Preliminary organic geochemical studies of samples from the Niger Delta (Nigeria). Analyses of crude oils for triterpanes. Chemical Geology, 27, 11-29. Evans, A. , 1990. Miocene sandstone provenance relations in the Gulf of Suez. Insight into synrift unroofing and uplift history.

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