It is shown in this note that the three methods, the orthonormalization method, the minor matrix method and the recursive reflection-transmission matrix method are closely related and solve the numerical instability in the original Thomson-Haskell propagator matrix method equally well. Another stable and efficient method based on the orthonormalization and the Langer block-diagonal decomposition is presented to calculate the response of a horizontal stratified model to a plane, spectral wave. It is a numerically robust Thomson-Haskell matrix method for high frequencies, large layer thicknesses and horizontal slownesses. The technique is applied to calculate reflection-transmission coefficients, body wave receiver functions and Rayleigh wave dispersion. © 2012 The Seismological Society of China and Springer-Verlag Berlin Heidelberg.
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Ma, Y., Wang, R., & Zhou, H. (2012). A note on the equivalence of three major propagator algorithms for computational stability and efficiency. In Earthquake Science (Vol. 25, pp. 55–64). https://doi.org/10.1007/s11589-012-0831-9