This report summarizes the recent work of scientists involved with bro
ad-band seismic studies in South Africa. Eight portable broad-band sei
smic stations were deployed throughout the Archaean Kaapvaal Craton fo
r a period of eighteen months to assist in defining lateral variations
in the underlying crust and upper mantle. The studies undertaken comp
rised: spectral ratio analysis, delay time modelling waveform inversio
n, shear-wave splitting, and mantle converted phases. All the data obt
ained during the broad-band lithospheric project clearly indicate that
within the Kaapvaal Craton there are major geological features sugges
ting that the craton is not a homogeneous entity. The large-scale feat
ures of the western portion of the craton show anomalous deep structur
es, different from any structures that have yet been reported in areas
of Archaean age.