| 000 | 02680cam a2200349 a 4500 | ||
|---|---|---|---|
| 003 | EG-GiCUC | ||
| 005 | 20250223032203.0 | ||
| 008 | 190210s2018 ua dhb 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.2018.Mo.R | ||
| 100 | 0 | _aMostafa Mohamed Omar Mohamed Hassan Elwakil | |
| 245 | 1 | 0 |
_aRare elements signature of stream sediments of East Wadi Karim, South West Quseir, Eastern Desert, Egypt / _cMostafa Mohamed Omar Mohamed Hassan Elwakil ; Supervised Ahmed A. Elkammar , Yasser Medhat Abdelrahman , Mohammad Fathy Abdelfattah |
| 246 | 1 | 5 | _aبصمة العناصر النادرة فى الرواسب الوديانية : شرق وادي كريم : جنوب غرب القصير الصحراء الشرقية : مصر |
| 260 |
_aCairo : _bMostafa Mohamed Omar Mohamed Hassan Elwakil , _c2018 |
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| 300 |
_a92 Leaves : _bcharts , facsimiles , maps ; _c30cm |
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| 502 | _aThesis (M.Sc.) - Cairo University - Faculty of Science - Department of Geology | ||
| 520 | _aHamadat area represents the catchment zone of an elliptical diaper-like intrusion pluton trending NNW-SSE. This pluton is one of the granitic diaper series exposed along the road that have yielded ages between 590 and 597 Ma. It is composed mainly of K-feldspar (22-52 vol.%), plagioclase (13-45 vol.%), quartz (19-39 vol.%), and biotite (up to 12 vol.%). Based on this modal composition, it is classified as monzogranite and it is highly jointed and exfoliated. Pegmatite and quartz veins and pods dissect it. It is also considered as homogenous, in terms of composition. Riebeckite-bearing granite is recorded in the northwestern segment of the pluton and it is composed mainly of perthite (up to 55%), quartz (35-40%), albite (5-15%), riebeckite (<5%) and biotite (<5%) and commonly sheared and highly silicified. The recorded non-opaque heavy minerals in the studied stream sediments include biotite, hornblende, riebeckite, epidote, and garnet, together with the accessory minerals; zircon, rutile, titanite, tourmaline, monazite and xenotime. Thorite, allanite, monazite, zircon, and apatite are recorded in the heavy mineral fraction as REE-bearing minerals | ||
| 530 | _aIssued also as CD | ||
| 653 | 4 | _aArabian-Nubian Shield | |
| 653 | 4 | _aHeavy mineral | |
| 653 | 4 | _aNon-opaque | |
| 700 | 0 |
_aAhmed A. Elkammar , _eSupervisor |
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| 700 | 0 |
_aMohammad Fathy Abdelfattah , _eSupervisor |
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| 700 | 0 |
_aYasser Medhat Abdelrahman , _eSupervisor |
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| 856 | _uhttp://172.23.153.220/th.pdf | ||
| 905 |
_aNazla _eRevisor |
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| 905 |
_aShimaa _eCataloger |
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| 942 |
_2ddc _cTH |
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| 999 |
_c70063 _d70063 |
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