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Abstract A worldwide collection of 25 sets of velocity and density measurements from adjacent shales, brine sands, and gas sands was acquired with full-waveform sonic, dipole sonic, and conventional well logging devices and/or in the laboratory. These data provide theoretical shale over brine-sand and shale over gassand P-wave and S-wave normal-incidence reflection coefficients (RP and RS), AVO intercepts (A), AVO gradients (B), the AVO indicators RP — RS (reflection coefficient difference), and A * B (AVO product). The reflection coefficient difference is found to be a more universal indicator than the AVO product in clastic stratigraphic intervals. For shale over brine-sand reflections, the average RP — RS tends to be near zero and relatively invariant with depth. Irrespective of gas-sand impedance, RP — RS is always negative for shale over reservoir quality gas-sand reflections and more negative than for the corresponding brine-sand reflections. In comparison, the AVO product may be positive, near zero, or negative for gas-sands depending on the impedance contrast with the overlying shale. These measurements also verily that RP — RS is well approximated by a simple linear combination of A and B.