Internal deformation due to shear and tensile faults in a half-space
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...D elastic half-space dislocation model [Okada, 1992] to best fit the observed two horizontal components of GPS velocity at each site around the area....
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...…assume that the crustal deformation of the northeastern plateau is dominated by deep slip of a series of major active faults which are approximated as simple dislocation segments locked 20 km to the surface and slipping below to an infinite depth in an elastic half-space [Okada, 1992] (Figure 8)....
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...[30] As a tentative experiment, we assume that the crustal deformation of the northeastern plateau is dominated by deep slip of a series of major active faults which are approximated as simple dislocation segments locked 20 km to the surface and slipping below to an infinite depth in an elastic half-space [Okada, 1992] (Figure 8)....
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...(rather than dip slip) and strike-slip rates for each of the faults using a 3-D elastic half-space dislocation model [Okada, 1992] to best fit the observed two horizontal components of GPS velocity at each site around the area....
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"Internal deformation due to shear a..." refers background in this paper
...The remaining term, U/B(Xl, X2,0), reduces to the formula for the surface displacement field due to a point force in a half-space (Okada, 1985)....
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...In a previous paper (Okada, 1985), we have obtained a complete set of compact closed analytical expressions for the surface deformation due to inclined shear and tensile faults in a half-space....
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"Internal deformation due to shear a..." refers methods in this paper
...If we take the Cartesian coordinate system, as shown in Figure 1, uJ(xl, x 2, xa; }1, }2, }3), the ith component of the displacement at ( x 1, x 2, x 3) due to the jth direction point force of magnitude F at (~1, ~2, 43) can be rewritten from the formula by Mindlin (1936) or Press...
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