--> Potential Field Analysis of the East African Rift in Eastern Tanzania—Guiding Seismic Survey Planning
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Previous HitPotentialNext Hit Previous HitFieldNext Hit Analysis of the East African Rift in Eastern Tanzania—Guiding Seismic Survey Planning

Abstract

Recent oil discoveries in the Kenyan Lokichar Basin, on the eastern branch of the East African Rift System, indicate more extensive oil Previous HitpotentialNext Hit within the rift systems than previously thought. A combination of legacy aeromagnetic Previous HitdataNext Hit together with proprietary airborne gravity and magnetic surveying over the Kilombero Trough, Kilosa Basin, Kidatu Basin and Pangani Basin in eastern Tanzania provided the base geophysical datasets to investigate the Previous HitpotentialNext Hit for thick accumulations of Tertiary and or Karoo sediments within these sections of the eastern branch of the rift. Previous geological investigations suggested basin depths of 2 km to 8 km are possible in the region. The objective of the Previous HitpotentialNext Hit Previous HitfieldNext Hit surveys was to identify thicker prospective sections of the Tertiary basins for evaluation by seismic surveying. Regional structural interpretation of the legacy aeromagnetic Previous HitdataNext Hit identified major long-lived fault systems controlling intra-rift basin development, and provided a qualitative assessment of depth-to-basement, constituting a significant advance in the understanding of the basin evolution than could be gleaned from satellite spectral and topographic Previous HitdataNext Hit. Naudy and Previous HitEulerNext Hit automated depth-to-basement methods were employed in conjunction with manual 2.5D forward modelling on the proprietary datasets to quantitatively evaluate basin depths and geometry. Using density contrasts typically expected for Precambrian basement, Karoo and Tertiary sequences, 2.5D forward modelling of the airborne gravity Previous HitdataNext Hit showed the Previous HitpotentialTop for up to 7 km of basin sediments within the rift, and highlighted the possibility of Tertiary rifting within the Kilombero Trough. Follow up 2D seismic work has confirmed the prospective basin geometry, and has identified intra-basin structures of exploration interest.