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| Figure 1.11: Model of a normal fault taken from seismic data and analyzed using the boundary element code Poly3D. In this illustration the fault has an irregular tipline and an irregular surface. The fault surface is divided into many small triangular boundary elements. Inset: Dip slip, UDS, and strike slip, USS, are constant on an element but vary from element to element to model the slip distribution on the fault. Reprinted from (Maerten et al., 2002) with permission from Elsevier. | ||||
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