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Fine structure of the lowermost crust beneath the Kaapvaal craton and its implications for crustal formation and evolution

✍ Scribed by Fenglin Niu; David E. James


Book ID
117094012
Publisher
Elsevier Science
Year
2002
Tongue
English
Weight
408 KB
Volume
200
Category
Article
ISSN
0012-821X

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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