| 000 | 01852cam a2200349 a 4500 | ||
|---|---|---|---|
| 003 | EG-GiCUC | ||
| 005 | 20250223030225.0 | ||
| 008 | 100505s2010 ua d 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 | _aCai01.12.16.M.Sc.2010.Mo.P | ||
| 100 | 0 | _aMohamed Hassan Mohamed Yousef | |
| 245 | 1 | 0 |
_aPalaeomagnetic and magnetic fabric studies on Wadi Dib ring complex, Northern Eastern Desert, Egypt / _cMohamed Hassan Mohamed Yousef ; Supervised Elsayed Mohamed Abdelrahman , Ahmed Abubakr Anmar |
| 246 | 1 | 5 | _aدراسة المغناطيسية القديمة و النسيج المغناطيسى لصخور معقد وادى دب الحلقى: الصحراء الشرقية الشمالية: مصر |
| 260 |
_aCairo : _bMohamed Hassan Mohamed Yousef , _c2010 |
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| 300 |
_a128 Leaves : _bcharts ; _c30cm |
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| 502 | _aThesis (M.Sc.) - Cairo University - Faculty of Science - Department of Geophysics | ||
| 520 | _aWadi (W.) Dib ring complex is represented by a perfect ring structure of about 2.3 km in diameter intruding a pre-existing precambrian synorogenic granodiorites. It is the only ring complex that is situated in the Northern Eastern Desert of Egypt. Yhe ring complex and its surrounding granodiorite rocks were sampled at 50 sites representing both the four main rock types forming the ring (alkaline syenite, quartz syenite, trachyte and pink granite) and the granodiorites | ||
| 530 | _aIssued also as CD | ||
| 653 | 4 | _aGeophysics | |
| 653 | 4 | _aPalaeomagnetic | |
| 653 | 4 | _aWadi Dib | |
| 700 | 0 |
_aAhmed Abubakr Anmar , _eSupervisor |
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| 700 | 0 |
_aElsayed Mohamed Abdelrahman , _eSupervisor |
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| 856 | _uhttp://172.23.153.220/th.pdf | ||
| 902 | _a1 | ||
| 905 |
_aMustafa _eRevisor |
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| 905 |
_aSamia _eCataloger |
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| 942 |
_2ddc _cTH |
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| 999 |
_c30202 _d30202 |
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