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In post-Pretoria Group times, but before the intrusion of the Bushveld Complex at -2050 Ma, the area surrounding the Fault zone underwent two compressive events.
The fault rocks within the Fault zone were also recrystallised, destroying any pre-existing tectonic fabric.
It is thought that the crystallisation of the Bushveld Complex has rheologically strengthened the neighbouring strata, preventing them from being refaulted.
Thickness differences in the Daspoort Formation of the Pretoria Group on opposite sides of the Fault suggest that the Fault was active during Pretoria Group sedimentation, with normal faulting producing localised second-order basins on the down-thrown side of the Fault.
striking Rustenburg Fault zone, in the western Transvaal Basin, South Africa, has been mapped, in order to unravel its tectonic history.
After the intrusion of the Bushveld Complex, little movement has occurred along the Fault, especially where the Fault passes under areas occupied by the Bushveld Complex.
Locally, the Fault zone has been assimilated by the Bushveld Complex.
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