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dc.contributor.authorKibirige, Gideon
dc.date.accessioned2020-01-13T11:16:01Z
dc.date.available2020-01-13T11:16:01Z
dc.date.issued2019-06
dc.identifier.urihttp://hdl.handle.net/20.500.12281/8432
dc.descriptionThis report is submitted to the department of geology and petroleum studies in partial fulfillment for the award of bachelors of Science degree in petroleum geosciences and production in the college of natural sciences, Makerere Universityen_US
dc.description.abstractA field work and excursion study to the Albertine graben under the guidance of our lecturers during the recess term of third year of our study for 14 days. The area of study was Semliki basin located in the southern part of the Albertine graben in Uganda. The study area lies onshore south of Lake Albert, it is bounded by an escarpment to the east and south and River Semliki to the west. 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 studies. 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).en_US
dc.language.isoenen_US
dc.publisherMakerere Universityen_US
dc.subjectGeologyen_US
dc.subjectGeophysicsen_US
dc.subjectAlbertine Grabenen_US
dc.subjectSemiliki areaen_US
dc.subjectNtoroko districten_US
dc.subjectWestern Ugandaen_US
dc.titleGeology and geophysics fieldwork report of the Albertine Graben, Semliki Area, Ntoroko District, Western Ugandaen_US
dc.typeThesisen_US


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