Expressions identical to the formulas of a preceding paper are obtained when due allowance is made for the variation of quantities which were erroneously taken as constant. A method for the approximate inversion of the travel-time curves is presented for the case where the surfaces of equal velocity are planes with an infinitesimal dip.

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First page of Travel-time equations and energy propagation for an elastic, heterogeneous, isotropic medium: Correction and approximate inversion
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