The
original data obtained from the reference line are computed
and rotated to their real spatial position by a reorientation
process in 3 steps.
The
data are first plotted on a stereonet for each reference line
respectively.
The
second step consist of reprocessing of all the stereonet in
order to place in a parallel orientation all the reference planes.
After this operation, clear trends appear for tectonic and sedimentary
planes.
The
original data obtained from the reference line are computed
and rotated to their real spatial position by a reorientation
process in 3 steps.
