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008 190918s2019 ua dh f m 000 0 eng d
040 _aEG-GiCUC
_beng
_cEG-GiCUC
041 0 _aeng
049 _aDeposite
097 _aPh.D
099 _aCai01.12.15.Ph.D.2019.Ra.C
100 0 _aRania Saeid Ismaeil Morsy Abuali
245 1 0 _aChemostratigraphy and paleo-environments of the upper cretaceous {u2013} lower tertiary sedimentary sequence in Safaga area, Red Sea, Egypt /
_cRania Saeid Ismaeil Morsy Abuali ; Supervised Ahmed Mohamed Abdelaziz Elkammar , Jochen Kuss , Moataz Mohamed Adel
246 1 5 _aالكيمياء الطبقية والبيئات القديمة للتتابع الرسوبي الطباشيري العلوي والثلاثي بمنطقة سفاجا : الصحراء الشرقية : مصر
260 _aCairo :
_bRania Saeid Ismaeil Morsy Abuali ,
_c2019
300 _a146 P. :
_bcharts , facsimiles ;
_c25cm
502 _aThesis (Ph.D.) - Cairo University - Faculty of Science - Department of Geology
520 _aThe Upper Cretaceous-Lower Tertiary sedimentary sequences in the Central Eastern Desert of Egypt were studied in three shallow boreholes (Wassief, Um El-Huaitat, and Mohamed Rabah). This study focuses on an integrated investigation of biostratigraphy, lithostratigraphy, petrography and geochemical (inorganic and organic) parameters, to provide important clues to interpret the prevailed depositional conditions. Biostratigraphically, eight planktonic foraminiferal zones, ranging in age from Late Cretaceous to Early Eocene were documented; Globotruncana aegyptiaca, Parasubbotina pseudobulloides, Praemurica trinidadensis, Praemurica uncinata, Morozovella angulata, Globanomalina pseudomenardii, Morozovella velascoensis, and Morozovella subbotinae zones. Three hiatus surfaces were recognized as evidenced by missing some formaniniferal zones. Petrographically, thirteen Microfacies Types (MFT) were recognized; MFT-1, silty to sandy mudstone; MFT-2, organic-rich silty mudstone; MFT-3, fine-grained sandstone/glauconite intercalations; MFT-4, phosclast packstone to phosclast grainstone; MFT-5, phosooid packstone to phosooid grainstone; MFT-6, non-fossiliferous lime-mudstone; MFT-7, phosphatic foraminiferal pack/grainstone; MFT-8, bioclastic foraminiferal packstone, MFT-9, bioclastic foraminiferal wackestone; MFT-10, glauconitic phosphatic foraminiferal wack-packstone; MFT-11, non-fossiliferous dolomitic mudstone; MFT-12, dolomitic glauconitic lime-mudstone, and MFT-13 dolomitic bioclastic wackestone
530 _aIssued also as CD
653 4 _aBiostratigraphy
653 4 _aLate Cretaceous-Early Eocene boundaries
653 4 _aLithostratigraphy
700 0 _aAhmed Mohamed Abdelaziz Elkammar ,
_eSupervisor
700 0 _aJochen Kuss ,
_eSupervisor
700 0 _aMoataz Mohamed Adel ,
_eSupervisor
856 _uhttp://172.23.153.220/th.pdf
905 _aNazla
_eRevisor
905 _aShimaa
_eCataloger
942 _2ddc
_cTH
999 _c73994
_d73994