000			03509cam a2200349 a 4500
003			EG-GiCUC
005			20250223031611.0
008			161112s2016 ua dh 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.2016.Mo.P
100	0		_aMohamed Adel Ibrahim Khalil
245	1	0	_aPlio-pleistocene tectono-stratigraphy, reservoir facies and hydrocarbon accumulation in Northeastern Nile Delta, Egypt / _cMohamed Adel Ibrahim Khalil ; Supervised Abdelmoneim Ahmed Elaraby , Ahmed Niazy Elbarkooky , Amr Hassan Elewa
246	1	5	_aالوضع التكتونى - الأستراتيجريفى و السحنى و تأثيره على التجمعات الهيدروكربونية لخزان البليو - بليوستوسين للجزء الشمالى الشرقى من دلتا النيل: مصر
260			_aCairo : _bMohamed Adel Ibrahim Khalil , _c2016
300			_a272 P. : _bcharts , facsimiles ; _c25cm
502			_aThesis (M.Sc.) - Cairo University - Faculty of Science - Department of Geology
520			_a The Tertiary Nile Delta is considered as one of the most important hydrocarbon gas provinces in Egypt with several giant gas fields and a great potential for more future discoveries. The present study addresses the Plio-Pleistocene tectono-stratigraphic framework and its impact on the hydrocarbon accumulation in northeastern Nile Delta. It sheds more light on the geological and petrophysical aspects of the Low Resistivity Low Contrast (LRLC) intervals (i.e. heterolithic levee facies) of the investigated reservoirs, which are usually overlooked during conventional reservoir evaluation procedures. Seismic attributes combined with DHIs (Direct Hydrocarbon Indicators) and conventional seismic interpretation are utilized to identify shallow gas targets in the area. This study is based on biostratigraphic, 3D seismic and wireline log data from seven wells distributed in the study area.The study area is divided into three tectono-stratigraphic sectors based on structural framework interpretation that are; (1) southern un-deformed sector, (2) central sector, and (3) northern sector. Each sector has its own stratigraphic, structural and gas potential characteristics. The integration of geological and seismic data revealed that the Plio-Pleistocene sedimentary regime and reservoir distribution are influenced and framed by three main NW trending structural lines.The Plio-Pleistocene reservoirs (Kafr El Sheikh and El Wastani formations) were deposited in the middle to distal parts of a turbidite system including turbidite lobes and channel-levee complexes. These could be seismically detected and confirmed from the facies analysis using core description and wireline logs interpretation along with borehole image data analysis. Consequently, three main facies associations could be identified: (1) massive thick bedded sandstone facies (stacked lobes), (2) channel fill deposits facies, and (3) heterolithic levee facies (low resistivity reservoirs)
530			_aIssued also as CD
653		4	_aDHIs
653		4	_aListric faults
653		4	_aTectono-stratigraphy
700	0		_aAbdelmoneim Ahmed Elaraby , _eSupervisor
700	0		_aAhmed Niazy Elbarkooky , _eSupervisor
700	0		_aAmr Hassan Elewa , _eSupervisor
856			_uhttp://172.23.153.220/th.pdf
905			_aNazla _eRevisor
905			_aShaima _eCataloger
942			_2ddc _cTH
999			_c58547 _d58547