In light of the foregoing analogy, the stress-intensity factors ki, kt for an isotropic and transversely isotropic solid differ only in that v is replaced by 1 -fi/a.Since k% and kt are independent of the shear modulus ju, there is no need to redefine the constants A and B as it was done in equations (1) and (2) of the discussion. Furthermore, it is the opinion of the authors that the discusser did not provide the pertinent information in his work [1] for finding the expressions of ki and kz-Incidentally, the derivation of h? and kz from the crack-border stress field, based on the limiting forms of the elliptical coordinates (£, T], f) to the polar coordinates (r, 6), is by no means an easy task.