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Structural style of the Turkana Rift, Kenya

Journal Article · · Geology; (United States)
Multifold seismic reflection and geologic mapping in part of the eastern branch of the East African Rift system of northern Kenya reveal a major rift structure containing at least 3 km of Neogene sediment fill beneath Lake Turkana. This includes a series of half-graben basins, with centrally located quaternary volcanic centers, which are linked end-to-end by structural accommodation zones. Whereas the geometry of rifting is similar to that of the nonvolcanic western branch of the East African Rift system, the Turkana half-grabens are much smaller and may reflect extension of a thinner lithosphere or development of more closely spaced fracture patterns during rift evolution, or both.
Research Organization:
Duke Univ., Durham, NC (USA)
OSTI ID:
6939199
Journal Information:
Geology; (United States), Journal Name: Geology; (United States) Vol. 16:3; ISSN GLGYB
Country of Publication:
United States
Language:
English

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