| dc.description.abstract | A field work and excursion study to the Albertine graben under the guidance of our lecturers during the recess term of third year was conducted for 10 days. The area of study was Semliki basin located in the southern part of the Albertine graben in Uganda.
The Albertine Graben is one of the most petroliferous onshore rifts in Africa. It forms the northernmost termination of the western arm of the East African Rift System.The Semliki Basin is covered by sediments that represent the Middle Miocene to Recent, which are described from outcrop and well data, underlain by possible Jurassic or Permo-Triassic to Early Tertiary sediments, which rest unconformably on Basement, described from seismic data.
The aim of this study was to enable us apply the geological, geophysical and other knowledge we have acquired during the course of the program to understand the geology, scrutinize and analyze the petroleum system of the area practically; then make conclusions whether the petroleum system is working or not. While carrying out the field work studies, environments of deposition as well as the depositional processes that took place in the area through the critical analysis of the stratigraphy and structures of the sediments were studied.
Vast structural and stratigraphic data collected were then analyzed to make conclusions about the petroleum potential of Semliki basin. Many different facies types were identified in the area, as well as their significance in the formation of good reservoir rocks and seals. The basin was affected by intensive tectonic activity, that led to the formation of vast types of structures with in the basement and sediments that were observed. Examples of these structures include faults and folds. Sedimentary structures such as mud diapirs, faults, plunging folds (anticlines) would be good structural traps for petroleum. The presence of hot springs with in the area indicated the presence of high enough thermal gradients for oil maturation. According to the Turaco well geophysical logs that were interpreted, the sediments were thick enough and are comprised of alternating layers of thick sand stones over lain by clays. These geophysical logs also showed the presence of hydrocarbons due to the cross overs observed between the neutron porosity and density logs. It was concluded that the study area had a good petroleum system (working petroleum play).
The sediments in the Semliki Basin represent a petroleum play for hydrocarbon accumulations, in which the necessary elements of a valid petroleum system were identified. These include excellent or good potential for reservoirs and top seals as well as circumstantial evidence of regionally mature source rocks, possible seals, traps and hydrocarbon-migration pathways. | en_US |
