Subsurface Images of the Eastern Rift, Africa, from the Joint Inversion of Body Waves, Surface Waves, and Gravity: Investigating the Role of Fluids in Early-Stage Continental Rifting.
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Geophysical Journal International
Abstract
The Eastern Rift System (ERS) of northern Tanzania and southern Kenya, where a cratonic
lithosphere is in the early stages of rifting, offers an ideal venue for investigating the roles of
magma and other fluids in such an environment. To illuminate these roles, we jointly invert
arrival times of locally recorded P and S body waves, phase delays of ambient noise generated
Rayleigh waves and Bouguer anomalies from gravity observations to generate a 3-D image
of P and S wave speeds in the upper 25 km of the crust. While joint inversion of gravity and
arrival times requires a relationship between density and wave speeds, the improvement in
resolution obtained by the combination of these disparate data sets serves to further constrain
models, and reduce uncertainties. The most significant features in the 3-D model are (1) P
and S wave speeds that are 10–15 per cent lower beneath the rift zone than in the surrounding
regions, (2) a relatively high wave speed tabular feature located along the western edge of the
Natron and Manyara rifts, and (3) low (∼1.71) values of Vp/Vs throughout the upper crust,
with the lowest ratios along the boundaries of the rift zones. The low P and S wave speeds
at mid-crustal levels beneath the rift valley are an expected consequence of active volcanism,
and the tabular, high-wave speed feature is interpreted to be an uplifted footwall at the western
edge of the rift. Given the high levels of CO2 outgassing observed at the surface along border
fault zones, and the sensitivity of Vp/Vs to pore-fluid compressibility, we infer that the low
Vp/Vs values in and around the rift zone are caused by the volcanic plumbing in the upper crust
being suffused by a gaseous CO2 froth on top of a deeper, crystalline mush. The repository for
molten rock is likely located in the lower crust and upper mantle, where the Vp/Vs ratios are
significantly higher.

