000			02951cam a2200337 a 4500
003			EG-GiCUC
005			20250223032032.0
008			180816s2017 ua dh f m 000 0 eng d
040			_aEG-GiCUC _beng _cEG-GiCUC
041	0		_aeng
049			_aDeposite
097			_aM.Sc
099			_aCai01.12.16.M.Sc.2017.Am.I
100	0		_aAmina Ramadan Abdelhalim
245	1	0	_aIntegrated interpretation of the aerial gamma-ray spectrometric, magnetic and remote-sensing data, Kadabora area, Eastern Desert, Egypt / _cAmina Ramadan Abdelhalim ; Supervised Khaled Soliman Soliman , Abdelmohsen Galal Nady Gharieb
246	1	5	_aالتفسير المتكامل للمعطيات الإشعاعية الطيفية والمغناطيسية و الفضائية لمنطقة كادابورا : الصحراء الشرقية : مصر
260			_aCairo : _bAmina Ramadan Abdelhalim , _c2017
300			_a172 P. : _bcharts , facsimiles ; _c25cm
502			_aThesis (M.Sc.) - Cairo University - Faculty of Science - Department of Geophysics
520			_aThe study area is located at the central part of the Eastern Desert of Egypt, and is mainly cropped out by different varieties of Precambrian basement rocks represented by younger and older granites; epidiorites, metavolcanics and metasediments. In the present study, statistical analyses are used to divide the different lithological units into normal distribution units and interpreted radiolithologic subunits (IRLSU), according to their radiometric characters. 41 IRLSU were identified. According to the computations and the results of application of the statistical inference tests, the new four Abu Lijam Diorite-Metagabbro IRL subunits (gd-14n1, gd-14n2, gd-14n3 and gd-14n4) and the new Older Granite subunit (go-15n) was extracted. Magnetic data was interpreted with the integration of surface and subsurface geological information to explain the main structural trends and tectonic basement map by using a Geosoft and lineament analysis software package. By using the Euler depth and second vertical methods, the depth of the study area was estimated. Through the application of the principle component analysis on the spectrometric data (eU, eTh, K% and their ratios of the three elements eU/K, eU/eTh& eTh) with the 6 bands of the Landsat ETM image we find that, the PC3 is loaded by the higher value of eU/eTh, so it was called spectrometric component and ensure the results of the statistical analysis and were represented in the form of color composite image to delineate the geologic boundaries
530			_aIssued also as CD
653		4	_aAeroradiospectrometry
653		4	_aCentral Eastern Desert
653		4	_aKadabora area
700	0		_aAbdelmohsen Galal Nady Gharieb , _eSupervisor
700	0		_aKhaled Soliman Soliman , _eSupervisor
856			_uhttp://172.23.153.220/th.pdf
905			_aNazla _eRevisor
905			_aShimaa _eCataloger
942			_2ddc _cTH
999			_c67098 _d67098