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- W269728599 abstract "Southern Africa contains the second largest elevated plateau on Earth, however despite decades of study the evolution of the “African Superswell” remains poorly understood. The mantle anomaly beneath Southern Africa provides a mechanism that can account for both the distribution and the amount of uplift observed, however the timing of uplift cannot be constrained from models of mantle flow because of uncertainties in density and viscosity parameters in the convection models. In order to improve the models of topographic evolution in response to mantle convection, and improve our understanding of the coupling between mantle flow and dynamic topography at the surface we require better quantitative constraints on relatively modest (∼1 km) long wavelength surface uplift." @default.
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- W269728599 date "2010-05-01" @default.
- W269728599 modified "2023-09-23" @default.
- W269728599 title "Dating the emergence of the Africa Superswell: a window into mantle processes using combined (U-Th)/He and AFT thermochronology" @default.
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