By M. Younes
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Application of isotope type curves to multiple source rock correlation in the Gulf of Suez, Egypt. Abstract, American Association of Petroleum Geologist Bulletin, 61, 631. 2 Hydrocarbon Potentials in the Northern Western Desert of Egypt M. A. Younes Geology Department, Moharrem Bek, Faculty of Science, Alexandria University, Alexandria, Egypt 1. Introduction The Western Desert of Egypt covers two thirds of the whole area of Egypt. The coastal basins (Matruh, Shushan, Alamein and Natrun) located in the northern half of the Western Desert 75 kilometers to the southwest of Matruh City, covering an area of about 3800 Km2 which forms the major part of the unstable shelf as defined by Said (1990).
And the locations of Khatatba, Alam El-Bueib and Abu Roash-G source rocks. Fig. 7. Relation between HI and TOC and the locations of Khatatba, Alam El-Bueib and Abu Roash-G source rocks. 31 Hydrocarbon Potentials in the Northern Western Desert of Egypt 7. Source rock extracts Two types of extracts can be identified in this study on the basis of the saturate/aromatic and the pristine/phytane ratios. Type (A) includes Abu Roash-G and Alam El-Bueib while, type (B) represents Khatatba Formation (Table 2).
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.