Crustal and Upper Mantle Structure Beneath Kimberley: Constraints From Body Wave Conversions Using a Dense Seismic Array.

As part of the Kaapvaal Craton Project (e.g.,<br>de Wit et al., 1992; Carlson et al., 1996), a<br>closely packed array of 32 broadband seismic<br>stations was deployed near the town of<br>Kimberley in December 1998, and was<br>operational for a period of seven months (Fig.<br>1).