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Bulletin of the Seismological Society of America; April 1970; v. 60; no. 2; p. 317-320
© 1970 Seismological Society of America
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Inversion of the spherical layer-matrix

TA-LIANG TENG

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 M–1 is obtained. Using Wronskians and recurrence relations of the spherical Bessel functions, it is shown that the inverse matrix M–1 can be simplified enough to insure an improvement in economy and accuracy in machine computations. Some useful properties of the inverse matrix M–1 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.
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