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Fault-related Soil Efflux of Mantle-derived CO2 in the Magadi and Natron Basins, East African Rift
(University of Nairobi, 2014)
The Magadi (Kenya) and Natron (Tanzania) basins of the East African Rift are in an early stage (< 7 Ma) of continental rifting. The many normal faults observed in these areas create sediment-filled basins and a large number ...
Contribution of transverse structures, magma, and crustal fluids to continental rift evolution: the East African rift in southern Kenya
(2013-12-13)
The Magadi rift in southern Kenya formed at ~7 Ma within Proterozoic rocks of the Mozambique orogenic belt, parallel to its contact with the Archean Tanzania craton. The rift is bounded to the west by the ~1600-m-high ...