9:00 AM - 9:15 AM
[SEM14-11] Can electrical conductivity help us understand the earthquake-induced stress-cycle in the ductile region beneath the Alpine Fault, New Zealand?
★Invited Papers
Keywords:Electical conductivity, Ductile deformation, Mylonitization
However, the mechanism by which the enhanced conductivity is produced at mid-crustal depths is poorly understood. Based on observations of the fault rocks being exhumed along the Alpine Fault we think that the most plausible mechanism is pressure-solution-creep associated with the latter stages of fault rock mylonitization. The dissolution-precipitation chemistry at the grain boundaries would provide additional charge carriers enhancing the conductivity of the grain boundary fluid and explain the correlation observed between the conductivity and the surface strain rate.
Since creep depends on differential stress, the question that arises is whether it would be possible to turn the conductivity image into a stress image. This will only be possible if we have a clear understanding of the mechanisms producing the conductivity and deformation. Laboratory-based studies of the electrical properties of materials undergoing ductile deformation at mid-crustal temperatures and pressures are needed to develop this understanding. However, if the relationship between the conductance and creep rate can be established we would have a new way of assessing the stress in the ductile region beneath the Alpine Fault and thus a new window into the mechanics of the earthquake cycle.