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Mantle structure and composition to 800-km depth beneath southern Africa and surrounding oceans from broadband body waves
(Elsevier Science Ltd. www.elsevier.com/locate/lithos, 2003)
Average one-dimensional P and S wavespeed models from the surface to depths of 800 km were derived for the southern
African region using travel times and waveforms from earthquakes recorded at stations of the Kaapvaal and ...
Pn arrivals and lateral variations of Moho geometry beneath the Kaapvaal craton
(Elsevier Science Ltd. www.elsevier.com/locate/lithos, 2003)
Pn arrivals from mining-induced earthquakes on the edge of the Witwatersrand basin show that the P wavespeeds in the
uppermost mantle are almost constant throughout most of the Kaapvaal craton. The presence of only small ...
South African seismicity, April 1997 to April 1999, and regional variations in the crust and uppermost mantle of the Kaapvaal craton
(Elsevier Science Ltd. www.elsevier.com/locate/lithos, 2003)
Events induced by deep gold-mining activity on the edge of the Witwatersrand basin dominate the seismicity of South
Africa. The deployment of 54 broad-band seismic stations at 84 separate locations across southern Africa ...
The P wavespeed structure below and around the Kaapvaal craton to depths of 800 km, from traveltimes and waveforms of local and regional earthquakes and mining-induced tremors
(Oxford University Press, https://academic.oup.com/gji, 2002-10-01)
An average P-wavespeed model from the surface to depths of 800 km was derived for southern Africa using traveltimes and waveforms from earthquakes recorded at stations of the Kaapvaal and South African National networks. ...