For antiplane shear, the only nonzero infinitesimal strains are and . Their trace is zero. The isotropic constitutive law consequently giveswith every other component zero. The first two equations of motion vanish because the fields are independent of . The third is , henceThe PDF omits the final equals-zero; this is the equation supplied by momentum balance.
For a steadily moving field put and . In the subsonic case , the equation becomes . With it reduces to . Thus is a harmonic function and, on a simply connected region, has a harmonic conjugate; there is a holomorphic function such thatThis is steadily moving antiplane shear. The representation is local on more general domains unless the conjugate's periods vanish. The subsonic condition is essential: at or above the shear-wave speed the coordinate rescaling is degenerate or the equation is hyperbolic rather than this elliptic harmonic problem.
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