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Fault-controlled fluid migration during early-stage continental rifting in the Magadi Basin, Kenya
(University of Nairobi, 2014)
The mechanisms controlling the migration of mantle-derived, CO2-rich fluids in early-stage continental rifts are poorly constrained, yet have important implications for processes occurring during the initiation of continental ...
Rift initiation with volatiles and magma
(University of Nairobi, 2015)
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 ...