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DEPARTMENT OF GEOLOGICAL SCIENCES UNIVERSITY OF SOUTHERN CALIFORNIA, LOS ANGLES, CALIFORNIA
Abstract
In their formulation of wave problems in a spherically layered medium, Phinney and Alexander have arrived at a layer-matrix M which forms the fundamental building block of their solution. In actual application of the theory, the inversion of M is needed for each assumed spherical shell. Since numerical inversion of the matrix M may introduce undesired accumulation of errors, an analytical inverse matrix M1 is obtained. Using Wronskians and recurrence relations of the spherical Bessel functions, it is shown that the inverse matrix M1 can be simplified enough to insure an improvement in economy and accuracy in machine computations. Some useful properties of the inverse matrix M1 are discussed which reduce the amount of machine time even further.
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S. N. BHATTACHARYA Rayleigh waves from a point source in a spherical medium with homogeneous layers Bulletin of the Seismological Society of America, February 1, 1978; 68(1): 231 - 238. [PDF] |
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