Constraining mantle density structure using geological evidence of surface uplift rates: The case of the African Superplume
- 19 July 2000
- journal article
- Published by American Geophysical Union (AGU) in Geochemistry, Geophysics, Geosystems
- Vol. 1 (7)
- https://doi.org/10.1029/1999gc000035
Abstract
No abstract availableKeywords
This publication has 54 references indexed in Scilit:
- Role of temperature‐dependent viscosity and surface plates in spherical shell models of mantle convectionJournal of Geophysical Research, 2000
- Global high-resolution phase velocity distributions of overtone and fundamental-mode surface waves determined by mode branch strippingGeophysical Journal International, 1999
- Denudation and uplift at passive margins: the record on the Atlantic Margin of southern AfricaPhilosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences, 1999
- A degree 8 mantle shear velocity model from normal mode observations below 3 mHzJournal of Geophysical Research, 1999
- Evidence for strong shear velocity reductions and velocity gradients in the lower mantle beneath AfricaGeophysical Research Letters, 1998
- Joint seismic tomography for bulk sound and shear wave speed in the Earth's mantleJournal of Geophysical Research, 1998
- Simultaneous inversion for 3-D variations in shear and bulk velocity in the mantlePhysics of the Earth and Planetary Interiors, 1997
- Bounds on global dynamic topography from Phanerozoic flooding of continental platformsNature, 1990
- Interaction of mantle dregs with convection: Lateral heterogeneity at the core‐mantle boundaryGeophysical Research Letters, 1986
- Tertiary Sea-Level Movements around Southern AfricaThe Journal of Geology, 1981