Late Precambrian and Lower Palaeozoic palaeomagnetic results from South Australia and Western Australia

Seismic reflection and refraction data are described from four locations in the eastern Mediterranean. Over the Mediterranean Ridge the profiles reveal a great thickness of material in the velocity range 3.6 – 5.5 km/sec. The crust is very disturbed and so penetration is limited, but at the foot of the Nile Cone an unreversed line gives a depth to the mantle of 27 km. This suggests that the crust in the eastern Mediterranean is more likely to be continental than oceanic in structure.