In geology, aseismic creep or fault creep is measurable surface displacement along a Geologic fault in the absence of notable . Aseismic creep may also occur as "after-slip" days to years after an earthquake. Notable examples of aseismic slip include faults in California (e.g. Calaveras Fault, Hayward Fault, and San Andreas Fault).
Causes
Aseismic creep accommodates
Far field motions on localized zones of deformation at
Plate tectonics. The underlying causes of aseismic creep are primarily attributed to poor frictional strength of the fault, low
normal stress acting on the fault in the shallow crust, and excessive pore-fluid pressures, which limit the viable amount of
normal stress on a fault. The frictional reaction of geologic materials can explain the transition from seismic to aseismic deformation with depth.
Friction along faults can cause sudden slips with associated stress drops (
), along with phases of no motion as stress recharges.
Measurements
Knowing how creep rates vary temporally and spatially along faults has important implications for predicting the timing, locations, and potential sizes of future
as well as the mechanics of fault behavior. Measurements of inter-seismic strain, as well as the associated pattern of coupling, are also crucial because they reveal the pockets where stress is building up and may be released in future seismic ruptures.
The emergence of space-based geodesy and newly developed
remote sensing techniques are used to monitor
Orogeny in order to track aseismic creep on a fault.
surveys are used with alignment arrays to track the creep. These data may then be used to restrict a fault's seismic capacity.
Examples
Aseismic creep exists along the
Calaveras Fault in Hollister,
California. Streets crossing the fault in Hollister show significant offset. Several houses sitting atop the fault are notably twisted, yet still habitable. The city attracts geologists and geology students almost weekly.
Other examples of faults that have experienced aseismic creep include a San Andreas Fault in California and the North Anatolian Fault in Turkey.
See also
External links
