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dc.contributor.authorNakudo, Ronnie Hillary
dc.date.accessioned2023-02-10T13:33:12Z
dc.date.available2023-02-10T13:33:12Z
dc.date.issued2022-10-27
dc.identifier.citationNakudo, R. H. (2022). Geological mapping project report of area h, Igayaza-Isingiro district from 30/01/2022 to 08/02/2022. (MakUD). (Unpublished Undergraduate technical report). Makerere University, Kampala, Uganda.en_US
dc.identifier.urihttp://hdl.handle.net/20.500.12281/15680
dc.descriptionSubmitted to the Department of Geology and Petrolatum Studies Makerere University in partial fulfillment of the award of Bachelor of Science degree in Geology.en_US
dc.description.abstractThe Gayaza mapping project is carried out by second year undergraduate students of Geology and petroleum geoscience and production at the department of geology and petroleum studies at Makerere University. The project is aimed at giving the students hands on training in geological mapping techniques, data collection and analysis, presentation of the geological data and report writing. The study area is Gayazain Isingiro district in Western Uganda. This area is part of the karagwe-Ankolean system of rocks which is the name given to the rocks of the Kibaran belt in Uganda. The area is divided into areas with each area assigned to a group of students. The mapped area which is fully discussed in this report is area H. Thearea was traversed while making observations of rock units, mineralogy and structures at the same time taking measurements on attitudes of the different geological structures. Samples were also taken and thin sections created. The thin sections were analyzed in the laboratory under petrographic microscopes. The measurements taken were analyzed using stereonet software to interpret the orientation of the different geological features. A base map of area H was also produced in the field and this was digitized using Arch GIS software to produce the geological map of the area. The field observations identified grey shales, ferruginous shales and quartzites as the rock units n area H. The rocks also contain quartz and iron oxide veins. The major minerals include quartz, casts, and faults. The folds are both regional and cross folds. A new theory is also proposed for feldspars, clay minerals and biotite. The major structures include joints, folds, bedding, load the events that formed the two fold trends.en_US
dc.language.isoenen_US
dc.publisherMakerere University.en_US
dc.subjectStratigraphyen_US
dc.subjectRock Structures
dc.subjectLithology
dc.subjectArea H, Igayaza-Isingiro district
dc.titleGeological mapping project report of area h, Igayaza-Isingiro district from 30/01/2022 to 08/02/2022.en_US
dc.typeTechnical Reporten_US


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