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Initiation of the western branch of the East African Rift coeval with the eastern branch

Roberts, Eric M; Stevens, N. J; O'Connor, Patrick M; Dirks, P.H.G.M; Gottfried, Michael D; Clyde, W. C; Armstrong, Richard; Kemp, A.I.S; Hemming, S


The East African Rift System transects the anomalously high-elevation Ethiopian and East African plateaux that together form part of the 6,000-km-long African superswell structure. Rifting putatively developed as a result of mantle plume activity that initiated under eastern Africa. The mantle activity has caused topographic uplift that has been connected to African Cenozoic climate change and faunal evolution. The rift is traditionally interpreted to be composed of two distinct segments: an...[Show more]

CollectionsANU Research Publications
Date published: 2012
Type: Journal article
Source: Nature Geoscience
DOI: 10.1038/ngeo1432


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