000			03061cam a2200337 a 4500
003			EG-GiCUC
005			20250223032407.0
008			190928s2018 ua dhb 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.2018.Ma.G
100	0		_aMahmoud Mohamed Ahmed Mostafa
245	1	0	_aGeological modeling and sedimentological architecture of Cenomanian- Upper Albian Sequence in East Tiba Half Graben, North Western Desert, Egypt / _cMahmoud Mohamed Ahmed Mostafa ; Supervised Mohamed Darwish Mohamed Salem , Selim Saber Selim
246	1	5	_aبناء نموذج جيولوجي و رسوبى لتتابع عصر السينومينى- الألبى العلوى لحوض شرق طيبة المخسوف، شمال الصحراء الغربية، مصر
260			_aCairo : _bMahmoud Mohamed Ahmed Mostafa , _c2018
300			_a89 P. : _bcharts , facsimiles , maps ; _c25cm
502			_aThesis (M.Sc.) - Cairo University - Faculty of Sciences - Department of Geology
520			_aIn 2005, the importance of East Tiba Sub-Basin was highlighted since the oil was commercially discovered for the first time in the Upper Albian Lower Bahariya sandstones. All the used available subsurface data including cores, sedimentary structures, lithological characters, wireline logs signature, petrophysical parameters and biostratigraphy have revealed that, the Lower Bahariya reservoir sandstones are represented by three main stacked tidal channels that were deposited in marginal marine possible tidal-dominated estuary depositional environment. A regional conceptual depositional model has been constructed covering the development leases and surrounding areas to understand the distribution of the sandy facies, their own petrophysical characters and related production behaviour.The model explained the inter-tonguing relations between the relatively low sand qualities (distal facies), less oil productive reservoir sands of the Shebl area sands and the good quality (proximal facies), more oil productive reservoir sands of the SE located marginal marine tidal channels of Shahd/Shahd SE Fields. A 3D reprocessed PSDM seismic cube has been used in addition to the well data to produce the Bahariya structure map as it represents a good seismic marker allover the study area. The play concept in the study area is a three way dip closure along NW trending Cretaceous faults having enough throw (+/- 600 ft.) to bring the Abu Roash 2G3 shales in the down-thrown side to juxtapose the Lower Bahariya reservoir sands in the up-thrown side
530			_aIssued also as CD
653		4	_aCenomanian- Upper Albian Sequence
653		4	_aEast Tiba Half Graben, North Western Desert, Egypt
653		4	_aShahd/Shahd SE fields
700	0		_aMohamed Darwish Mohamed Salem , _eSupervisor
700	0		_aSelim Saber Selim , _eSupervisor
856			_uhttp://172.23.153.220/th.pdf
905			_aNazla _eRevisor
905			_aShimaa _eCataloger
942			_2ddc _cTH
999			_c74172 _d74172