NOTES:

The analyses of FaultKin and Michael [1984] were found to be quite similar.
We chose all locations where there was quality outcrop to take measurements. At first, we planned to do a transect across the fault, but lack of quality outcrop made this impossible.
The number of faults measured ranged from 15 to 35. A total of 128 faults were measured in all.
Stress orientations varied at each location.
We combined the six data sets together to get an overall stress field orientation.
The results are shown in the following diagrams.