History of the development of Permian-Cretaceous rifts in East Africa: a series of interpreted maps through time

摘要

East Africa represents the most rifted portion of crust on the planet, having been subjected to numerous phases of extension from Permian to Recent times. The first rifting phase commences in the Permian as the 'Karoo' set of narrow half-graben, many formed by lateral shear. Peak rifting appears to be of Middle Permian age for rifts south of Tanzania. In Kenya, Ethiopia and Somalia, this rift population merges into a set of rifts with peak rifting of earliest Triassic age.