000			02124cam a2200337 a 4500
003			EG-GiCUC
005			20250223031033.0
008			140903s2013 ua h 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.2013.Ah.M
100	0		_aAhmed Abdelhady Mohamed Soliman
245	1	0	_aModeling of depositional environment and sequence stratigraphy of AbuMadi reservoir, Elwastani Field, West Elmanzala concession, onshore Nile Delta, Egypt / _cAhmed Abdelhady Mohamed Soliman ; Supervised Abdel Moneim Alaraby , Almoataz Bellah Hassouba
246	1	5	_aنموذج للب{u٠٦أأ}ئات الترس{u٠٦أأ}ب{u٠٦أأ}ة و طبق{u٠٦أأ}ة التتابع لخزان ابو ماضى لحقول الوسطانى: غرب المنزلة: دلتا نھر الن{u٠٦أأ}ل: مصر
260			_aCairo : _bAhmed Abdelhady Mohamed Soliman , _c2013
300			_a145 P. : _bfacsimiles ; _c25cm
502			_aThesis (M.Sc.) - Cairo University - Faculty of Science - Department of Geology
520			_aThe AbuMadi reservoirs are the main producers in the Nile Delta. In this study the complex geology of a fluvial deltaic near shore system was modeled using the concepts of sequence stratigraphy to build the basic reservoir architecture for the AbuMadi reservoir. Two depositional cycles were recognized based on implementing the sequence stratigraphy concept. These are: Lower AbuMadi cycle (3.3) and Upper AbuMadi cycle (3.4). Lower AbuMadi sand reservoir is believed to have been deposited in braided fluvial channel system at the base followed upwards by tidal near shore marine environment during latter phase of marine transgression.
530			_aIssued also as CD
653		4	_aAbuMadi reservoir
653		4	_aDepositional environment
653		4	_aSequence stratigraphy
700	0		_aAbdel Moneim Alaraby , _eSupervisor
700	0		_aAlmoataz Bellah Hassouba , _eSupervisor
856			_uhttp://172.23.153.220/th.pdf
905			_aNazla _eRevisor
905			_aSamia _eCataloger
942			_2ddc _cTH
999			_c47152 _d47152