Abstract
AP-wave velocity model for the upper mantle beneath eastern and southern Africa is proposed. The top 250 km of the model is characterized by relatively low velocities similar to those deduced for the upper mantle beneath the western United States of America. At greater depths, the velocities gradually change to normal mantle values.
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Green, A.G. An upper mantleP-wave velocity model for eastern and southern Africa. PAGEOPH 116, 1262–1273 (1978). https://doi.org/10.1007/BF00874685
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DOI: https://doi.org/10.1007/BF00874685