000 | 02022cam a2200349 a 4500 | ||
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003 | EG-GiCUC | ||
005 | 20250223030226.0 | ||
008 | 100509s2010 ua dh f m 000 0 eng d | ||
040 |
_aEG-GiCUC _beng _cEG-GiCUC |
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041 | 0 | _aeng | |
049 | _aDeposite | ||
097 | _aPh.D | ||
099 | _aCai01.12.15.Ph.D.2010.Ah.M | ||
100 | 0 | _aAhmed Farouk Mohamed Abuelenein | |
245 | 1 | 0 |
_aMediterranean seafloor - outer offshore Nile Delta : _bMorpho - sedimentological and environmental assessment / _cAhmed Farouk Mohamed Abuelenein ; Supervised Mohamed Darwish Salem , Ahmed Nyazi Elbarkooky |
246 | 1 | 5 |
_aقاع البحر المتوسط فى القطاع البحرى الخارجى لدلتا النيل : _bمورفولوجية الترسيب والتقييم البيئى |
260 |
_aCairo : _bAhmed Farouk Mohamed Abuelenein , _c2010 |
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300 |
_a184P. : _bcharts , facsimiles ; _c30cm |
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502 | _aThesis (Ph.D.) - Cairo University - Faculty of Science - Department of Geology | ||
520 | _aUnderstating the shallow geology in the deepwater part of the Nile Deep Sea Fan (NDSF ) is tackled within the area of the Northeastern Mediterranean Deepwater concession (NEMed ) operated by Shell Egypt for hydrocarbon exploration . 3D seismic data and core data is used to study the shallow geology in two different scales . 3D seismic data and core data is used to study the shallow geology in two different scales . On the seismic scale Mass Transport Deposits (MTDs) is studied with the main focus on the Rosetta MTD (RMTD ) and the Sapphire MTD (SMTD ) in two seismic surveys within the NEMed concession named as the NEMed 2001 and the Kj 53 areas | ||
530 | _aIssued also as CD | ||
653 | 4 | _aDeepwater | |
653 | 4 | _aMTDs | |
653 | 4 | _aSapropels | |
700 | 0 |
_aAhmed Nyazi Elbarkooky , _eSupervisor |
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700 | 0 |
_aMohamed Darwish Salem , _eSupervisor |
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856 | _uhttp://172.23.153.220/th.pdf | ||
902 | _a1 | ||
905 |
_aFatma _eCataloger |
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905 |
_aMustafa _eRevisor |
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942 |
_2ddc _cTH |
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999 |
_c30239 _d30239 |