Terminologyforstructuraldiscontinuities GEOLOGICNOTE

A system with possible faults is modeled as a group of hidden Markov models representing the system in fault-free mode and different failure modes, and a first order Markov chain

Slip inversion means reconstructing the orientation and shape of the stress ellipsoid (finding the stress matrix) from measured fault slip data (the orientation of fault

Field observations suggest that the thin deformation bands are not restricted to the Moab Member fault damage zone at the Courthouse Branch Point.. Similar structures have also

The differences in the way that slip surfaces (faults) and deformation bands accumulate displacement with respect to length is shown here to have dramatic consequences for the fault

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As fault complexes in nature show the structures at their final state of deformation, the structural 

Figure 4-8: plots showing throw to displacement for faults from Foxford et al., 1998 (blue diamonds) and the observations from ANP that have been described in this paper

The exploration and rendering methods used in this paper, including transparent surfaces, cutting planes, object identification and removal, and ambient occlusion (which is a