000			02808cam a2200313 a 4500
003			EG-GiCUC
008			191208s2019 ua b 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.2019.Mo.T
100	0		_aMona Ibrahim Ahmed Faid
245	1	0	_aTectono-stratigraphic framework and hydrocarbon potentialities of East tiba sub-basin, North western desert, Egypt / _cMona Ibrahim Ahmed Faid ; Supervised Mohamed Darwish Mohamed Salem , Shawky Mohamed Mohamed Sakran
246	1	5	_aالإطار التكتونى الطباقى و الإمكانات الهيدروكروبونية للحوض الفرعى شرق طيبة: شمال الصحراء الغربية: مصر
260			_aCairo : _bMona Ibrahim Ahmed Faid , _c2019
300			_a147 P. : _bmaps ; _c25cm
502			_aThesis (M.Sc.) - Cairo University - Faculty of Science - Department of Geology
520			_aThe main objective of this study is to throw light on the stratigraphic and tectonic framework in addition to hydrocarbon-bearing sequences in East tiba sub-basin (ETSB). The study area is located to the northeast of Abu Gharadig basin, western desert, Egypt. The ETSB is evolved through a complex tectono-stratigraphic history with complex phases of tectonic evolution. It was initially as an intracratonic rift basin during the Early jurassic time and continued its subsidence throughout the cretaceous time and superposed by wrench tectonics during lattermost cretaceous and Early paleogene, with a NE oriented half-graben structural geometry. Detailed seismic interpretation using 3D seismic profiles integrated with a complete suite of the geological well data is applied to improve understanding the basin fill and its corresponding hydrocarbon potentiality. Constructed structure contour maps of significant seismic horizons regarding the near top Khoman, Abu Roash "C" and "F" members, Bahariya and Wadi Elnatrun formations. The study area underwent three main tectonic events superimposed each other: (1) extension related to the opening of the tethys during jurassic-early cretaceous with a direct impact on the presence and maturity of source rock and trap formation, (2) wrenching and inversion related to the closing of the tethys in the late cretaceous-early tertiary and (3) younger extensional phase that reactivated during the miocene and post-miocene age
530			_aIssued also as CD
653		4	_aAbu Gharadig
653		4	_aEarly jurassic-cretaceous intracratonic rift
653		4	_aEast tiba sub-basin
700	0		_aMohamed Darwish Mohamed Salem , _eSupervisor
700	0		_aShawky Mohamed Mohamed Sakran , _eSupervisor
905			_aNazla _eRevisor
905			_aSamia _eCataloger
942			_2ddc _cTH
999			_c75701 _d75701