TRACKING EFFICIENCY ASSOCIATED WITH FAULT SYSTEM REORGANIZATION IN LABORATORY AND NUMERICAL EXPERIMENTS
Between episodes of fault reorganization, fault systems may become less efficient as they produce increasing off fault deformation. For example, laboratory and numerical experiments show that the interference and interaction between different fault segments may increase local internal work or that increasing convergence can increase work against gravity produced by a fault system. This accumulation of work triggers fault reorganization. The internal work and work against gravity are conservative, so stored work produced in deforming the inefficient system provides the energy required to grow new faults that reorganize the system to a more efficient configuration.
The results of laboratory and numerical experiments reveal that we should expect crustal fault systems to reorganize following periods of increasing inefficiency, even in the absence of changes to the tectonic regime that loads the faults. The time frame of fault reorganization depends on fault system configuration, strain rate and processes that relax stresses within the crust. For example, stress relaxation may keep pace with stress accumulation, which limits the increase in the internal work and gravitational work so that irregularities can persist along active fault systems without reorganization of the fault system. Understanding the partitioning of the work budget through laboratory and numerical experiments can reveal the processes that govern fault reorganization to more optimal configurations.