(b)
Figure 3. An example, taken from ten Brink et al. (1996) of the use of the Beasy code in
a geophysical context. Here the displacements around strike slip faults that intersect the
surface of the earth are modeled. (A) The horizontal displacement of the earth due to a strile
slip fault. (B) The vertical displacement due to several interacting facults. The grid represents
deformation of the originally orthogonal mesh.
C-12