| 000 | 01824cam a2200349 a 4500 | ||
|---|---|---|---|
| 003 | EG-GiCUC | ||
| 005 | 20250223030804.0 | ||
| 008 | 130310s2012 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.2012.Mo.S | ||
| 100 | 0 | _aMohamed Mohamed Abdelfattah Abdou | |
| 245 | 1 | 0 |
_aStructural and basinal evolution of the central east onshore gulf of Suez rift segment-Egypt / _cMohamed Mohamed Abdelfattah Abdou ; Supervised Mohamed Abdelwahed Mohamed , Alvar Braathen , Gouda Ismail Abdelgawad |
| 246 | 1 | 5 | _aالتطور التركيبى و الحوضى للجزء الأوسط الشرقى اليابس لأخدود خليج السويس-مصر |
| 260 |
_aCairo : _bMohamed Mohamed Abdelfattah Abdou , _c2012 |
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| 300 |
_a322 P. : _bcharts , facsimiles ; _c25cm |
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| 502 | _aThesis (Ph.D.) - Cairo University - Faculty of Science - Department of Geology | ||
| 520 | _aThe present study deals with structural and basinal evolution of the Gulf of Suez rift in the area between Wadi Eltayiba and Wadi Sidri on the eastern side of the Suez rift aiming to construct different tectonic models that are corresponding to different tectonic events. The current study shows that the extensional faults are the main structural features in addition to the some localized revers faults; also the fault-related folds are well observed | ||
| 530 | _aIssued also as CD | ||
| 653 | 4 | _aRift | |
| 653 | 4 | _aStructure | |
| 653 | 4 | _aSuez | |
| 700 | 0 |
_aAlvar Braathen , _eSupervisor |
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| 700 | 0 |
_aGouda Ismail Abdelgawad , _eSupervisor |
|
| 700 | 0 |
_aMohamed Abdelwahed Mohamed , _eSupervisor |
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| 856 | _uhttp://172.23.153.220/th.pdf | ||
| 905 |
_aNazla _eRevisor |
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| 905 |
_aSamia _eCataloger |
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| 942 |
_2ddc _cTH |
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| 999 |
_c41941 _d41941 |
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