000			03016cam a2200349 a 4500
003			EG-GiCUC
005			20250223032918.0
008			220207s2021 ua db f m 000 0 eng d
040			_aEG-GiCUC _beng _cEG-GiCUC
041	0		_aeng
049			_aDeposite
097			_aM.Sc
099			_aCai01.12.15.M.Sc.2021.Mo.C
100	0		_aMohammed Omar Sayed Sultan
245	1	0	_aCharacterization of upper miocene reservoirs in the Northeastern onshore portion of the Nile Delta, Egypt / _cMohammed Omar Sayed Sultan ; Supervised Abdelmoneim Ahmed Abdelkader Elaraby , Ahmed Niazy Ebarkooky
246	1	5	_aخصائص خزانات الميوسين العلوى بالجزء الشمالى الشرقى من دلتا النيل البرية : مصر
260			_aCairo : _bMohammed Omar Sayed Sultan , _c2021
300			_a146 P. : _bcharts , facsimiles ; _c25cm
502			_aThesis (M.Sc.) - Cairo University - Faculty of Science - Department of Geology
520			_aThe Nile Delta is considered as the earliest known delta in the world. The Nile Delta covered by a thick sequence of Neogene clastic, which is considered as one of the most important gas provinces in Egypt. The actual exploration activities in Nile Delta started in 1963 and continuous until now. The main target of the present study is determination of the properties of Upper Miocene reservoirs that help us to predict the distribution and quality of these reservoirs. The study area is located in the northeastern part of the onshore Nile Delta, between Latitudes 31{u00B0} 12' 00" and 31{u00B0} 24' 00", and Longitudes 31{u00B0} 16' 00" and 31{u00B0} 38' 00". The present study focuses on using the available geological data, well log data and seismic data, to evaluate the Upper Miocene, Abu Madi and Qawasim reservoirs, through the interpretation and integration of the well log with seismic data, to find out the connections between the geological and geophysical deductions. The results confirm that, the sandstone content exists as a main lithology in the Upper Abu Madi and Qawasim sections, at Narges-1 and El Basant-1 wells. The best quality sandstone appears in the Upper Abu Madi section at Narges-1 well and in Qawasim section at the upper part of El Basant-1 well and the Lower part of Narges-1 well.The clastics in Abu Madi and Qawasim formations have good petrophysical properties, in which the northwestern part of the study area is the best area as net reservoir, effective porosity and quality for Abu Madi section and the eastern part is the best portion as net reservoir, effective porosity and quality for Qawasim reservoir
530			_aIssued also as CD
650		0	_aMiocene
653		4	_aMiocene
653		4	_aNortheastern
653		4	_aOnshore portion
700	0		_aAbdelmoneim Ahmed Abdel Kader Elaraby , _eSupervisor
700	0		_aAhmed Niazy Ebarkooky , _eSupervisor
856			_uhttp://172.23.153.220/th.pdf
905			_aNazla _eRevisor
905			_aShimaa _eCataloger
942			_2ddc _cTH
999			_c84139 _d84139