A roughly 70 km diameter circular feature buried beneath the Kalahari
sands in South Africa is revealed on regional aeromagnetic maps. Boreh
oles drilled into the centre of the structure intercept a similar to 2
50 m thick sheet of quartz norite, interpreted as an impact melt, whic
h overlies brecciated and shock; metamorphosed basement granite, Zirco
ns recovered from the quartz norite, yield U-Pb ages of 145 +/- 0.8 Ma
, and biotites provide Ar-Ar ages of 144 +/- 4 Ma, These data provide
strong evidence for the occurrence of a Late Jurassic impact crater (t
he Morokweng impact structure) similar to 100 m beneath the surface.