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Seismic Velocity and Q Structure of the Middle Eastern Crust and Upper Mantle from Surface-wave Dispersion and Attenuation

✍ Scribed by L. Cong <SUP>*, †</SUP>, B. J. Mitchell


Publisher
Springer
Year
1998
Tongue
English
Weight
549 KB
Volume
153
Category
Article
ISSN
0033-4533

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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