Results 161 to 170 of about 202,200,666 (205)
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Navigation in the Gulf of Suez

Journal of Navigation, 1977
The 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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The Petroleum Geology Of Ihe Gulf Of Suez

Offshore Technology Conference, 1978
ABSTRACT 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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Tectonic evolution of the Gulf of Suez and the Gulf of Aqaba

Tectonophysics, 1988
Abstract 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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Neotectonics of the Red Sea, Gulf of Suez and Gulf of Aqaba

2018
The 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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Residual Circulation in the Gulf of Suez, Egypt

Estuarine, Coastal and Shelf Science, 1998
Abstract 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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Seismic survey of Sinai and the Gulf of Suez

Geophysics, 1958
Abstract Outlines the program of seismic investigations in the Suez gulf-southwest Sinai peninsula region, Egypt, leading to the discovery of oil-bearing structures at Belayim (an anticlinal trap) and Feiran, Abu Rudeis, and Ekma (fault traps).
Pierre A. A. H. Masson, F. J. Agnich
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Sub-salt imaging in the Gulf of Suez

Geological Society, London, Special Publications, 1990
Abstract Sub-salt imaging on seismic data is a serious geophysical problem affecting exploration in the Gulf of Suez. Here, thick Miocene evaporite, shale and salt sequences with salt tectonics overlie rift structures involving pre-Miocene and Miocene oil-producing formations.
R. Zaki   +3 more
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Multiple Reflections And Head Waves In The Gulf Of Suez

Offshore Technology Conference, 1978
ABSTRACT 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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On The Prawn Fisheries in the Gulf of Suez, Egypt

2009
يكون الجمبري حوالي 13.7% من محصول الصيد الكلي في خليج السويس وهناك 11% من المصيد من الأنواع الكبيرة بينيس جابونيكس بيت ، بينيس سيمسلكاتس دي هان ، وبينيس لاتيسلكاتس كيشنوي ، والنوعان الصغيران حجماً وهما متيا بنيوبسس ستريديولانتس ألكوك وتراكيبينيس كيرفيروسترس ستمبسون يمثلان 2.7% فقط من المصيد .
Yassin, Mohamed H. محمد ياسين   +3 more
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Turbine-PDC Applications in the Gulf of Suez

Proceedings of Middle East Oil Show, 1987
Abstract GUPCO (Gulf of Suez Petroleum Company) is the largest operator in Egypt. The last 2-1/2 years activity level has been high, with an average of 10-12 rigs operating, and annual footage drilled in excess of 600,000' [183,000 m]. Straight hole turbodrills and polycrystalline diamond compact (PDC) bits have improved ...
D. C. Howard, J. C. Day, S. Mansour
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