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    • Crustal structure on the northeastern flank of the Kenya rift. 

      Prodehl, C; Jacob, A.W.B; Thybo, H; Dindi, E; Stangl, R (1994)
      The KRISP flank line E converges with the Kenya rift at an angle of about 45° and is approximately parallel to the older Anza graben to the north. The depth to the basement is almost zero along the entire onshore part of ...
    • The influence of pre-existing structures on the evolution of the southern Kenya Rift Valley — evidence from seismic and gravity studies 

      Birt, C.S; Maguire, P.K.H; Khan, M.A; Thybo, H; Keller, G.R; Patel, J (Department of Geology, University of Leicester, UKGeological Institute, University of Copenhagen, DenmarkDepartment of Geological Sciences, The University of Texas, USADepartment of Physics, University of Nairobi, Kenya, 1997)
      The Kenya Rift is an active continental rift that has developed since the Late Oligocene. Although a thermal origin for the rifting episode is indicated by the scale of volcanism and its relative timing with uplift and ...