Analysis of ground deformation of viscoelastic half-space

Analysis of ground deformation of viscoelastic half-space

Analysis of ground deformation of a viscoelastic half-space due to movement of an infinite creeping and a finite locked

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In geology, a fault is a planar fracture or discontinuity in a volume of rock across which there has been significant displacement as a result of rock-mass movement. Large faults within the Earth's crust result from the action of plate tectonic forces, with the largest forming the boundaries between the plates, such as subduction zones or transform faults. According to elastic rebound theory, the tectonic earthquakes are caused by sudden release of elastic strain energy stored in the strain rock mosses in some regions of the earth in the lithosphere by fracture or fault movement produced by su...