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Earthquakes Faults Bounded Rift Basins of South Sudan
Current Issue
Volume 5, 2018
Issue 2 (June)
Pages: 21-26   |   Vol. 5, No. 2, June 2018   |   Follow on         
Paper in PDF Downloads: 37   Since Jun. 5, 2018 Views: 1170   Since Jun. 5, 2018
Authors
[1]
Khalda Yassin Ibrahim, Department of Seismology, Remote Sensing and Seismology Authority, National Center for Research, Khartoum, Sudan.
[2]
Abd Alhafiz Gad El Mula, Department of Geology, Faculty of Science, Khartoum University, Khartoum, Sudan.
Abstract
The South Sudan rift system extends from the western part of Sudan (south Darfur), through the southern part of Kenya to join the fault system in the Indian. In the South Sudan, earthquake activity is reported from many localities in South Sudan, especially at Jebel El Rajaf, which frequent quakes. This study aims at finding out the relationship between the seismic activity and the faults bounded the rift basins. The gravity data is used to display the configuration of the rift basin which show clearly the existence of a rift in the study area. Four gravity initial models were constructed. These gravity models revealed that the depth of the basins ranges between 2 km to 4.5 km and the width ranges between 38 km to 72 km. The lineament features were created based on the geological map and landsat data. The areal distribution of seismic events is found to be associated with the lineaments in the southern flank of the basins. It will be concluded that the earthquakes in the study area are thought to be caused by the rejuvenation of faults bounding sedimentary basins.
Keywords
South Sudan, Rift Basins, Earthquakes, Gravity Data, Initial Models, Faults, Landsat Data and Lineaments
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