000			02108cam a2200337 a 4500
003			EG-GiCUC
005			20250223031353.0
008			151212s2015 ua hb 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.2015.Em.S
100	0		_aEman Hassan Salem
245	1	0	_aStructural synthesis of eastern part of Beni Suef Basin northeast Nile valley, Egypt / _cEman Hassan Salem ; Supervised Adel A. Sehim , Adel R. Moustafa
246	1	5	_a المزيج البنائى لمنطقة شرق حوض بنى سويف: شمال شرق وادى النيل: مصر
260			_aCairo : _bEman Hassan Salem , _c2015
300			_a148 P. : _bfacsimiles , maps ; _c25cm
502			_aThesis (M.Sc.) - Cairo University - Faculty of Science - Department of Geology
520			_aThe structural architecture of East Beni Suef Basin (EBSB) was studied using 3D seismic data and seven wells. The sedimentary fill of the basin is made up of Lower Cretaceous Kharita Formation, Upper Cretaceous Bahariya, Abu Roash, and Khoman Formations, Paleocene-Middle Eocene Apollonia Formation, Upper Eocene Maadi Formation and Post- Eocene sediments. Normal faults are the dominant structures in the basin. Three sets of faults were mapped; ENE-WSW fault set, NW-SE fault set, and NNW-SSE fault set. The EBSB was subjected to three main tectonic phases; The oldest (Early Cretaceous) tectonic phase was associated with the main extension and subsidence along the EBSB. The second phase was contemporaneous with the Late Cretaceous Syrian Arc deformation. The third tectonic phase took place during the Early Tertiary and was extensional
530			_aIssued also as CD
653		4	_aBeni Suef Basin
653		4	_aCretaceous-Eocene tectonics
653		4	_aSyrian arc tectonics
700	0		_aAdel Abdelaziz Sehim , _eSupervisor
700	0		_aAdel Ramadan Moustafa , _eSupervisor
856			_uhttp://172.23.153.220/th.pdf
905			_aNazla _eRevisor
905			_aSoheir _eCataloger
942			_2ddc _cTH
999			_c53909 _d53909