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This book investigates Wadi Fatima foldthrust belt in West Central Arabian Shield, East African Orogen. This belt involves the postamalgamation Fatima Group volcanosedimentary sequence that was deposited over a Neoproterozoic basement complex. The tectonic evolution of the whole Wadi Fatima District is discussed. The Fatima Group and the underlying basement rocks exhibit various structural elements due to the effect of the PanAfrican Orogeny. Geologic structures in the basement rocks are mainly transpressive. In Fatima Group, a wonderful geometric and kinematic relations between folding and thrusting are observed.
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