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For each FE model, displacement was calculated under the same loading and boundary conditions.
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A comparison of the GPS observations with the REF model displacements is presented in Figure 3.
The biggest problem in modeling displacements is usually stratigraphy and tectonics of the reservoir formation.
A stratified Cox regression model on fracture displacement was applied and adjusted for age, sex, quality of reduction, implant positioning, comorbidity, and walking disability.
The observed land displacement was modeled by viscoelastic rebound and afterslip on the mainshock fault (Ozawa et al. 2012; Sun et al. 2014; Diao et al. 2014; Silverii et al. 2014; Yamagiwa et al. 2015).
The two different models calculating lateral displacement are contact mechanics model and contact element model.
The model strain and displacement were obtained with a number of high-tech equipment such as high speed static strain test system, micro-precision grating displacement meter, digital cameras measuring systems, and high-precision total station test.
Two analytical models, 'Stress model' and 'Displacement model', were established from the ways of stress and displacement solution based on the modification of classical shear-lag model.
The approximate model assumes that transverse displacement is constant across the thickness.
And based on the approximate linearity of strain-magnetic field, second-order system model of the actuator displacement is established.
In this model, most of the displacement is accommodated in the fault core, which acts as a barrier to fluid movement.
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