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PROPAGATION OF ELASTIC WAVES IN LAYERED MEDIA BY ...

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376 BULLET<strong>IN</strong> <strong>OF</strong> THE SEISMOLOGICAL SOCIETY <strong>OF</strong> AMERICA(<strong>IN</strong>TERFACE)UPPERMEDIUMn=N-In=Nm-In=N+l -- 4- -I-tI, !-m-':' IIIII---1I. . . . III=-rn= I (<strong>IN</strong>TERFACE)n=2n=3LOWERMEDIUM(a)UPPERMEDIUM*(<strong>IN</strong>TERFACE)n:N-2 -- -n=N-In=Nm-III . . . . .Irn m+ln=l~r n---2---I-- - --IIIIIIIIIin=3LOWERMEDIUMZ(b)FzG. 5. Grid arrangement at the interface z = h. Part (a) shows the grid points used whenthe upper medium is extended to include an additional fictitious line below the interface, andpart (b) shows the grid points used when the lower medium is extended to include an additionalfictitious line above the interface.approximation. Equation (9) then becomes1 B 1 1 1 A 1 A 12~r [ .~+I,N,~ - Bm-I,N,~] + ~ [ m,~+l,~ -- m,~,~](#~)I1 2 B 2 1 A~ A2 1= ~ (B~+1,1,, - ~-~,1,,) + ~ ( ,~,~,,- ,~,~,,) • (25)

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