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Fig. 1.3.2.11 (a) Exterior of the central part of the FE model for f = 0.3. (b) Magnification of the ellipsoidal pressure source.

Fig. 1.3.2.12 For! = 1.

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Fig. 1.3.2.21 Confirmation of the precision of calcula- tion by the FE model of $ =#= 150 km ($ and# are the radius and the height of the FE model region, respectively). MogiYamakawas model (depth " = 10 km and radius%^!= 1 km) was reproduced by FEM.

Fig. 1.3.2.22 Ratio of the results of FE analysis to Yamakawas solution. A sufficiently high precision of calculation is realized.

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Fig. 1.3.2.31 Results of FE analysis for! = 0.2. Fig. 1.3.2.32 For! = 0.3.

Fig. 1.3.2.33 For! = 0.5. Fig. 1.3.2.34 For! = 0.25.

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Fig. 1.3.2.42 For" = 0.3.

Fig. 1.3.2.43 For" = 0.5. Fig. 1.3.2.44 For" = 0.7.

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