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S-wave velocity structure, mantle xenoliths and the upper mantle beneath the Kaapvaal craton

✍ Scribed by Angela Marie Larson; J. Arthur Snoke; David E. James


Book ID
108746937
Publisher
John Wiley and Sons
Year
2006
Tongue
English
Weight
686 KB
Volume
167
Category
Article
ISSN
0956-540X

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Travel times from earthquakes recorded at two seismic networks were used to derive an average P wavespeed model for the crust and upper mantle to depths of 320 km below southern Africa. The simplest model (BPI1) has a Moho depth of 34 km, and an uppermost mantle wavespeed of 8.04 km/s, below which t