Abstract Seven geological sections have been examined and sampled with emphasis on sedimentological & diagenetic processes within Abu Ghaylan Formation and the contact relationships with the underlying Abu Shaybah and overlying Kiklah Formations. Based on current detailed field loggings and microscope investigations, 10 facies are recognized within Abu Ghaylan Formation. The lowermost succession characterised by an overall transition from continental fluvially dominated deposits of the Abu Shaybah Formation into transitional to marginal marine, tidal flat deposits of the Abu Ghaylan Formation upward. The transitional nature of this lowermost part succession is demonstrated by interbeddings of claystone, sandstone and fossiliferous facies arranging in coarsening up cycle, in which most probably deposited in estuary / beach environment.The Abu Ghaylan Formation generally wedges laterally eastward and exposes intermittently east of Wadi Ghan area resulting of syngenetic uplift of Wadi Ghan area followed by erosion (ElHinnawy & Cheshitev, 1975). A slightly earlier uplift and greater erosion in a westward sloping basin of deposition near the close of the Early Jurassic and Early Cretaceous times is suggested by Fatmi & Sbeta (1991). The current study reveals that several exposure surfaces are demonstrated within Abu Ghaylan Formation suggesting uplifting and erosion episodes interrupted Abu Ghaylan Formation, where a restricted distribution of Abu Ghaylan may suggest a local tectonic overprint.Although the overall impression is that the base beds of Kiklah Formation starts with sandstone and red clay beds as channel infill deposits above Abu Ghaylan carbonate unit with surface of unconformity, however, based on current close investigation, a sequence characterized by interbeddings of carbonate and greenish clay overlying Abu Ghaylan Formation with surface of unconformity and gradationally overlain by sandstone beds should be introduced as separate unit attributes to Kiklah Formation.The current study emphasizes and supports a solution collapse origin for the breccias and introduces better insight into architecture and geomorphology of the breccias bodies that are exposed in the area of study. The dissolution of evaporites is considered responsible for all breccias development in this stratigraphic interval. According to the occurrence mode of breccias, the breccias intervals have been divided into two main parts; a lower section of strata that contains collapsed paleocaves and an upper section of strata that is deformed to varying degrees due to the collapse and compaction of the section of paleocave-bearing strata. The sharp flat base, inverse grading, V-shaped/ sag structures and irregular undulating top of brecciated bodies are recognized within Abu Ghaylan Formation and typically characterize solution collapse processes. Based on field study and architecture relationships, five distinctive karst facies are recognized in the area of study.The early diagenetic genetically related processes probably interrupted the deposition of Abu Ghaylan Formation is a most possible assumption for the origin and timing of breccias formation.
أحمد أبوبكر الحلو (2015)

فى هذه الدراسة تم تحديد خواص دالة هاملتون بإستخدام نمودج المفاعلة البوزونية IBM-2 وإيجاد أفضل البارامترات لدالة هاملتون وحساب قيم مستويات الطاقة وإحتمالية الإنتقال للنظائر Hg200-194، Kr90-84 ومقارنتها بالنتائج التجريبية والمحسوبة بطرق نظرية أخرى. Abstract In this study, we have determined the most appropriate Hamiltonian using the interacting boson model (IBM-2), and obtained the best fitting values of parameters to construct the Hamiltonian. We also have calculated the energy levels and the transition probabilities for Kr84-90and Hg194-200 and have compared the calculated values with experimental data and with the results of other calculations.
نجاة سالم الشفتري (2010)

ندرس في هذا البحث إحدى طرق التصوير بالرنين المغناطيسي، وهي طريقة الصدى المغزلي في بعدين. يحتوي هذا البحث علي ستة فصول، ففي الفصل الأول تم إعطاء لمحة تاريخية عن تقنية (MRI) بوجه عام، وفي الفصلين الثاني والثالث تمت المعالجة للأسس (MRI) الفيزيائية والرياضية، وفي الفصل الرابع تمت دراسة طريقة الصدى المغزلي في بعدين، وقد تم في الفصل الخامس إستعراض الدراسة العملية لحساب الإشارة المتحصل عليها لبعض الأنسجة (Tissue) بجسم الإنسان. وهذه الأنسجة هي: سائل النخاع الشوكي(Cerebrospinal Fluid). المادة البيضاء(White Matter). المادة الرمادية(Gray Matter). الورم(Tumor). لقد تم دراسة التباين(Contrast) لهذه الطريقة بإستخدام برنامج الحاسب بيئة(Math CAD)، وإستخدمت تحويلات فورييه السريعة(Fourier TransForm) لتحويل الإشارة المتحصل عليها من دالة في الزمن إلي دالة في التردد والمجال المتدرج. وتعرض النتائج المتحصل عليها في الفصل السادس.
زهرة علي العربي أبو راص (2014)