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Extra resources for Crude Oil Exploration in the World
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. Geochimica et Cosmochimica Acta , 45, 783-795. N. and Shehab, M. M. 1984. Petroleum generation, migration and occurrences in the Gulf off Shore of South Sinai, Proceeding of the 7 th Petroleum Exploration Seminar, 126-151, Cairo. Shanmugam, G. 1985.
Accordingly, these studies concluded that the stratigraphic section of the northern Western Desert contains multiple source rocks of different degrees of thermal maturation. The dark shale of Khatatba Formation that considered mature source rock with an excellent capability for both oil and gas generation. Shale rocks of Alam El-Bueib and Abu Roash-G formations considered a marginally to good mature source rock for oil generation during the Late Cretaceous. %), pyrolysis parameters (S1 and S2 values) and vitrinite reflectance measurements (Ro%) to evaluate their organic richness, kerogen types, and the degree of thermal maturity in the northern Western Desert of Egypt.
1953). Presence of certain trace metals particularly nickel and vanadium in crude oils is geochemically significant and provides information on the origin of crude oil. The work of Achi and Shide, 2004 revealed that Nigerian Bonny light crude and Bonny medium crude contains varying quantities of calcium, magnesium, zinc, iron, nickel, sodium and potassium in the following order: Na> Ca> Fe> Ni> Mg> >K >Zn in Bonny light crude while Bonny medium crude is of the order: Na> Ca> Fe> Ni> Mg> >K > Zn.