Digital Elevation Model (DEM) and wells data from the Rukwa Rift Basin has been used to define the evolution and timing of structural patterns within two structural domains: Domains A (north) and B (south). These structural domains are separated by the Saza Shear Zone (SSZ) which controls the oblique divergent effects of the Rukwa Rift. We demonstrate how these structures control the distribution of potential helium traps and reservoirs quality
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