Cf. Connors et al., CONSTRAINING NUMERICAL-MODELS WITH GEOMECHANICAL DATA AND MICROSEISMIC FAULT-PLANE SOLUTIONS, International journal of rock mechanics and mining sciences & geomechanics abstracts, 30(7), 1993, pp. 1371-1377
Geomechanical and seismic analyses are used to constrain interpretatio
ns based on a 3-D boundary element model (BEM) for different stages of
an excavation at depth. Mapping results indicate four dominant joint
sets throughout the rock mass Fault-plane solutions defined two potent
ial failure planes, one of which closely fits, in both strike and dip,
the mapped Stratigraphic Bedding set. BEM calculated principal stress
orientations compared well to the pressure, tension, and intermediate
axes obtained from the fault-plane solutions. Ubiquitous joint analys
es, with BEM derived shear/normal stresses for each joint set at the e
vent locations, indicate that only the Stratigraphic Bedding met the d
erived Barton-Bandis failure criteria Based on these correlations, it
is suggested that an integrated approach with seismic and geomechanica
l data can be used to constrain numerical stress analyses interpretati
ons.