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- W2549915512 abstract "Summary East Africa represents the most rifted portion of crust on the planet. The first rift phase commenced in the Permian as the ‘Karroo’ set of half grabens In Kenya and Ethiopia. These propagate into a set of younger rifts with peak rifting phases in the Early Triassic. A further phase of rifting is seen in the Early Jurassic, concentrated along what will later become the East African passive margin. This phase ends in the Kimmeridgian break-up between Africa and Madagascar. A Late Jurassic rift population also extends from Yemen across to Somaliland. Another population of latest Jurassic-earliest Cretaceous age is interpreted in onshore and offshore southern Mozambique. Multiphase Cretaceous rifting is concentrated along NW-SE trends. A focus in recent years has been the Anza Graben of Kenya, where events do not correlate well to the Sudan rifts. The East African Rift System (‘EARS’) commenced in the Lokichar Basins of northern Kenya in the Late Eocene to Oligocene. At various times during the Mid-Late Miocene, a series of small rifts and depressions formed between Ethiopia and Malawi, heralding the main regional rift subsidence phase and further rift propagation in the Plio-Pleistocene." @default.
- W2549915512 created "2016-11-30" @default.
- W2549915512 creator A5089351653 @default.
- W2549915512 date "2016-11-22" @default.
- W2549915512 modified "2023-09-23" @default.
- W2549915512 title "Tectonics and Petroleum Systems of East African Rifts" @default.
- W2549915512 doi "https://doi.org/10.3997/2214-4609.201602384" @default.
- W2549915512 hasPublicationYear "2016" @default.
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