User:Gabrielaperez544/Aseismic creep

In geology, aseismic creep or fault creep is measurable surface displacement along a fault in the absence of notable earthquakes. Aseismic creep may also occur as "after-slip" days to years after an earthquake. This article will analyze the major causes of aseismic creep, explain how measurements are taken, and provide prominent examples for a better explanation.

Causes
Through aseismic creep, most plate boundaries accommodate far-field motions on localized zones of deformation. 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 sliding which occurs in sudden slips with associated stress drops (earthquakes), 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 earthquakes as well as the mechanics of fault behavior. Inter-seismic strain measurement, 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 crustal deformation in order to track aseismic creep on a fault. Theodolite 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 and 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 the San Andreas Fault in California and the North Anatolian Fault in Turkey.