000 | 02241cam a2200337 a 4500 | ||
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003 | EG-GiCUC | ||
005 | 20250223031305.0 | ||
008 | 150906s2015 ua b f m 000 0 eng d | ||
040 |
_aEG-GiCUC _beng _cEG-GiCUC |
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041 | 0 | _aeng | |
049 | _aDeposite | ||
097 | _aM.Sc | ||
099 | _aCai01.12.15.M.Sc.2015.Ek.S | ||
100 | 0 | _aEkramy Ahmed Fawi Ali | |
245 | 1 | 0 |
_aStratigraphic and structural study on the early Pliocene reservoir, sapphire Field, Offshore Nile Delta- Egypt : _bwith special emphasis on the seismic amplitude attributes / _cEkramy Ahmed Fawi Ali;Supervised Elsayed Abdeaziz Aly Yousef , Mohamed Saleh Hassan Hammed |
246 | 1 | 5 | _aدراسة أستراتيجرافية و تركيبية لخزان البلايوسين السفلى حقل سافَير ، دلتا النيل البحرية {u٢٠١٣} مصر: مع التركيز الخاص على صفات السعة السيزمية |
260 |
_aCairo : _bEkramy Ahmed Fawi Ali , _c2015 |
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300 |
_a127 P. : _bmaps ; _c25cm |
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502 | _aThesis (M.Sc.) - Cairo University - Faculty of Science - Department of Geololgy | ||
520 | _aThe present thesis presents a structural and stratigraphic study on Sapphire Gas Field that lies in the West Delta Deep Marine (WDDM) concession. The thesis address the results of seismic reservoir mapping by identifying the different depositional architecture elements and model of the Early Pliocene reservoir of the Sapphire Field based on interpretation of Average Absolute Amplitude seismic (AAA) maps and their calibration with borehole data including the following. 1) Channels and channel fills i. Simple linear to highly sinuous sand fill channel (High amplitude) ii. Simple linear to highly sinuous mud fill channel (Low amplitude) iii. Channel Complex and Channel Fills - Laterally stacked channel complex system - Aggradational channel complex system | ||
530 | _aIssued also as CD | ||
653 | 4 | _aPliocene | |
653 | 4 | _aStratigraphic | |
653 | 4 | _aStructure | |
700 | 0 |
_aElsayed Abdelaziz Aly Yousef , _eSupervisor |
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700 | 0 |
_aMohamed Saleh Hassan Hammed , _eSupervisor |
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856 | _uhttp://172.23.153.220/th.pdf | ||
905 |
_aAml _eCataloger |
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905 |
_aNazla _eRevisor |
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942 |
_2ddc _cTH |
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999 |
_c52243 _d52243 |