The dip variant weights in the West Valley geodetic models have been halved (0.1, 0.3, and 0.1; 0.05 total weight in each geodetic model) suggesting this perhaps was slated to be considered a low probability of occurrence fault (see this issue for 2017). However, the change was never propagated through to the geologic model.
The dip variant weights in the West Valley geodetic models have been halved (0.1, 0.3, and 0.1; 0.05 total weight in each geodetic model) suggesting this perhaps was slated to be considered a low probability of occurrence fault (see this issue for 2017). However, the change was never propagated through to the geologic model.