Ejm. Willemse et Dd. Pollard, ON THE ORIENTATION AND PATTERNS OF WING CRACKS AND SOLUTION SURFACES AT THE TIPS OF A SLIDING FLAW OR FAULT, J GEO R-SOL, 103(B2), 1998, pp. 2427-2438
Sliding along a preexisting flaw can result in the formation of tensil
e cracks where stresses concentrate near the flaw tips. These tensile
cracks are referred to as wing cracks and are generally oriented obliq
ue to the preexisting flaw. Previous studies based on linear elastic f
racture mechanics (LEFM) showed that the kink angle depends on the rat
io of normal to shear loading on the flaw. We present analytical solut
ions for cohesive end zone (CEZ) flaw models and find that the relatio
nship between kink angle and load differs significantly from that for
LEFM flaws. Furthermore, the remote flaw-parallel normal stress may si
gnificantly reduce or increase the kink angle, especially for CEZ flaw
s with large end zones. These results suggest that multiple interpreta
tions are possible for: some measured kink angles. In some materials,
solution surfaces may form at the tip of the sliding flaw. By consider
ing the angle between wing cracks and solution surfaces it is possible
to determine whether the LEFM or CEZ model is more appropriate and th
us to provide a better constrained interpretation' of the boundary con
ditions that accompanied sliding. For some CEZ flaws the stress state
in the cohesive end zone is nearly homogeneous, possibly promoting for
mation of arrays of opening mode cracks and solution surfaces that tog
ether form a shear zone. The CEZ flaw model can explain some orientati
ons and patterns of cracks and solution surfaces commonly observed alo
ng natural faults that cannot be accounted for with the LEFM model.