M. Dragoni et al., A VISCOELASTIC SHEAR ZONE MODEL OF COMPRESSIONAL AND EXTENSIONAL PLATE BOUNDARIES, Pure and Applied Geophysics, 140(3), 1993, pp. 471-491
A model is proposed describing the mechanical evolution of a shear zon
e along compressional and extensional plate boundaries, subject to con
stant strain rate. The shear zones are assumed as viscoelastic with Ma
xwell rheology and with elastic and rheological parameters depending o
n temperature and petrology. Stress and strain are computed as functio
ns of time and depth. For both kinds of boundaries the model reproduce
s the existence of a shallow seismogenic zone, characterized by a stre
ss concentration. The thickness of the seismogenic layer is evaluated
considering the variations of shear stress and frictional strength on
faults embedded in the shear zone. Assuming that a fault dislocation t
akes place, the brittle-ductile transition is assumed to occur at the
depth at which the time derivative of total shear stress changes from
positive to negative values. The effects of different strain rates and
geothermal gradients on the depth of the brittle-ductile transition a
re studied. The model predictions are consistent with values inferred
from seismicity data of different boundary zones.