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Geological modeling and sedimentological architectures for the cenomanian sequences Khalda Ridge Area, North Western Desert, Egypt / Reda Wafdy Ibrahim Mohamed ; Supervised Ahmed M. Abukhadrah , Selim Saber Selim

By: Contributor(s): Material type: TextTextLanguage: English Publication details: Cairo : Reda Wafdy Ibrahim Mohamed , 2019Description: 184 P. : charts , facsimiles , maps ; 25cmOther title:
  • نمذجة جيولوجية وطرز الترسيب لتتابعات السينومانى: منطقة حافة خالدة: شمال الصحراء الغربية: مصر [Added title page title]
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  • Issued also as CD
Dissertation note: Thesis (M.Sc.) - Cairo University - Faculty of Science - Department of Geology Summary: The litho-stratigraphic cross sections, thickness variations and lithofacies of the Upper Bahariya reservoir (Upper Bahariya Member) are discussed to distinguish the shape, the extent of sedimentary basins and the environment of deposition. The studied Upper Bahariya reservoir shows that the Upper Bahariya Member top is coming higher at Yasser-06 well than the other three wells, which lies in the northeastern part of the study area. Furthermore, the maximum thickness of the Bahariya Formation occurs at Hayat-12, while the minimum thickness occurs at Hayat-17 well. The facies triangle lithologic model of the Upper Bahariya Member shows, the predominance of calcareous shale facies in most of the studied wells which change to shaley sand in the central part at Hayat-12 and Hayat-14 wells. These facies reflect a shallow marine environment grading from tidal-dominated estuarine channels to wave-dominated shoreline associating with lagoons or bays. The petrographic analysis shows that, there is a variation in the reservoir quality based on the detrital clay components and diagenetic processes
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Thesis Thesis قاعة الرسائل الجامعية - الدور الاول المكتبة المركزبة الجديدة - جامعة القاهرة Cai01.12.15.M.Sc.2019.Re.G (Browse shelf(Opens below)) Not for loan 01010110081182000
CD - Rom CD - Rom مخـــزن الرســائل الجـــامعية - البدروم المكتبة المركزبة الجديدة - جامعة القاهرة Cai01.12.15.M.Sc.2019.Re.G (Browse shelf(Opens below)) 81182.CD Not for loan 01020110081182000
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Cai01.12.15.M.Sc.2019.Mo.T Tectono-stratigraphic framework and hydrocarbon potentialities of East tiba sub-basin, North western desert, Egypt / Cai01.12.15.M.Sc.2019.Na.O Organic geochemical evaluation of the Oligocene Rocks East Abu Madi Onshore Field, Nile Delta, Egypt / Cai01.12.15.M.Sc.2019.Na.O Organic geochemical evaluation of the Oligocene Rocks East Abu Madi Onshore Field, Nile Delta, Egypt / Cai01.12.15.M.Sc.2019.Re.G Geological modeling and sedimentological architectures for the cenomanian sequences Khalda Ridge Area, North Western Desert, Egypt / Cai01.12.15.M.Sc.2019.Re.G Geological modeling and sedimentological architectures for the cenomanian sequences Khalda Ridge Area, North Western Desert, Egypt / Cai01.12.15.M.Sc.2020.Ah.G Geological applications of the space-borne (optical-radar) and ground penetrating radar (GPR) data in the shallow structures mapping and site investigation along the central part of Cairo Suez District, Egypt / Cai01.12.15.M.Sc.2020.Ah.G Geological applications of the space-borne (optical-radar) and ground penetrating radar (GPR) data in the shallow structures mapping and site investigation along the central part of Cairo Suez District, Egypt /

Thesis (M.Sc.) - Cairo University - Faculty of Science - Department of Geology

The litho-stratigraphic cross sections, thickness variations and lithofacies of the Upper Bahariya reservoir (Upper Bahariya Member) are discussed to distinguish the shape, the extent of sedimentary basins and the environment of deposition. The studied Upper Bahariya reservoir shows that the Upper Bahariya Member top is coming higher at Yasser-06 well than the other three wells, which lies in the northeastern part of the study area. Furthermore, the maximum thickness of the Bahariya Formation occurs at Hayat-12, while the minimum thickness occurs at Hayat-17 well. The facies triangle lithologic model of the Upper Bahariya Member shows, the predominance of calcareous shale facies in most of the studied wells which change to shaley sand in the central part at Hayat-12 and Hayat-14 wells. These facies reflect a shallow marine environment grading from tidal-dominated estuarine channels to wave-dominated shoreline associating with lagoons or bays. The petrographic analysis shows that, there is a variation in the reservoir quality based on the detrital clay components and diagenetic processes

Issued also as CD

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