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Tracer tests provide a mean to dynamically characterize the conduit or barrier behavior of the fault.
In turn, these are thought to affect the behavior of the fault and the size of the next quake, because strong rock with few cracks will unleash more energy when it fractures in an earthquake.
By fitting any physical example into this categorization based on the ratio of fault zone components, one can qualitatively describe the fluid flow behavior of the fault, which varies between these endmembers (Caine et al. 1996).
Ide (2014) proposed a hierarchical structure over a wide range of heterogeneities, including a characteristic large asperity and small SSE patches, which implies that the upper and lower limits of the hierarchical structure (i.e., the size of the largest and smallest patches) might control the overall behavior of the fault slip.
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A fault detection filter that simulates the behavior of the fault-free, reduced-order model is designed, and its discrepancy from the behavior of the actual process state estimates is used as a residual for fault detection.
The continuously yielding joint model was used to describe the non-linear behavior of the faults.
The authors analyzed fractures on outcrop scale which could be used to understand the hydraulic behavior of the faults.
The variability of radon gas concentrations due to seismic activity along a fault plane boundary shows positive results related to the stress and strain behavior of the faults.
Behavior of the active fault, as determined by the AIST, is plotted by the color segments that are defined in the legend.
Temperature is one of the key state parameters controlling the seismogenic behavior of the plate boundary fault zones (e.g., Hyndman et al. 1995; Moore and Saffer 2001).
Studies on the slipping behavior of the San Andreas Fault, however, suggest that it is not merely creeping but it rather consists of creeping patches, which build up stress on patches with high friction.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com