Results 121 to 130 of about 2,869 (168)
Egyptian Journal of Petroleum, 2017 The Semi-enclosed Suez Gulf records various signals of high anthropic pressures from surrounding regions and the industrialized Suez countries. The sedimentary hydrocarbons have been studied in 6 coastal stations located in the Gulf of Suez. Non-aromatic
Omayma E Ahmed, Mohamed M El Nady
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Egyptian Journal of Petroleum, 2018 Eight crude oils collected from different oilfields distributed within the northern, central and southern Gulf of Suez basin to detect the distribution of triterpanes and steranes biomarkers as indication of organic matter input and depositional ...
Mohamed A Ebiad +2 more
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Drilling Of Gulf Of Suez Evaporites
Middle East Technical Conference and Exhibition, 1979Abstract The Miocene evaporites of Gulf of Suez area comprise salt, anhydrite and, rarely, gypsum. They are mainly found south of 29 deg. N latitude line. Salt pillows and diapirs are common in the southern half pillows and diapirs are common in the southern half of Gulf of Suez and may be associated with upward ...
F. Khalaf, El H.M.
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Geothermal studies in oilfield districts of Eastern Margin of the Gulf of Suez, Egypt
NRIAG Journal of Astronomy and Geophysics, 2014 Results of geothermal studies carried out at 149 onshore oil wells have been used in evaluation of temperature gradient and heat flow values of the eastern shore of the Gulf of Suez.
Mohamed Abdel Zaher, Essam Ghamry
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Navigation in the Gulf of Suez
Journal of Navigation, 1977The need to improve and regulate navigation in the Gulf of Suez became urgent when the Suez Canal was reopened in June 1975, and urgency increased with the number and size of ships passing through the Canal. In 1975 the Suez Canal Authority embarked on a three-phase development operation over a period of six years; the first phase, completed in 1976 ...
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Tectonic evolution of the Gulf of Suez and the Gulf of Aqaba
Tectonophysics, 1988Abstract The tectonic evolution of the Gulfs of Suez and Aqaba can be determined using fault slip data. Early opening of the Suez rift in the lower Miocene resulted from NNE-SSW extension, oblique to the rift trend. Subsequent tectonic events began in the Late Burdigalian and were associated with ENE-WSW extension which determined the shape of the ...
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The Petroleum Geology Of Ihe Gulf Of Suez
Offshore Technology Conference, 1978ABSTRACT The present-day Gulf of Suez Basin was initiated during the Oligocene as a result of relative motion between the Arabian, Nubian, and Sinai plates. At that time, pre-Miocene sediments were broken into fault blocks that were rotated and then inundated by the organically rich "globigerina" marls and shales of
John E. Bobbitt, Jay O. Gallagher
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Residual Circulation in the Gulf of Suez, Egypt
Estuarine, Coastal and Shelf Science, 1998Abstract A three-dimensional non-linear hydrodynamical numerical model has been used to study the water movement in the shallow Gulf of Suez at the northern end of the Red Sea. The computational grid used to schematize the Gulf has a horizontal resolution of 3×3 km and levels at 5, 15, 30 and 60 m in the vertical.
M.A. Rady +3 more
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Neotectonics of the Red Sea, Gulf of Suez and Gulf of Aqaba
2018The Red Sea, Gulf of Suez, and Gulf of Aqaba comprise the active plate boundaries that separate Africa-Nubia, Arabia and Sinai. This tripartite configuration has been in existence since the Middle Miocene, or about the past 12–14 Ma. We describe the ongoing and geologically recent tectonics of these regions. The Red Sea rift lies east of a broad region
William Bosworth +2 more
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Multiple Reflections And Head Waves In The Gulf Of Suez
Offshore Technology Conference, 1978ABSTRACT Inferior reflection quality in the Gulf of Suez at the objective depth interval is attributable in part to surficial multiple reflections. An excellent example of the latter is observed on a typical seismic line in the northern portion of the Gulf.
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