Specify the amplitude convention. For normal-stress/pressure amplitudes, the seismic reflection coefficient and seismic transmission coefficient are
For particle displacement or velocity resolved in one fixed normal coordinate, the reflected amplitude changes sign and the transmitted ratio is instead
These are alternative conventions, not conflicting energy predictions. The reflected and transmitted energy flux fractions are
which sum to one for the ideal lossless interface. Thus an amplitude transmission coefficient greater than one does not violate conservation of energy.
Specify the amplitude convention. For incident stress/pressure amplitude one, the normal-incidence seismic reflection coefficient and stress seismic transmission coefficient are
At limestone–sandstone, and . At sandstone–salt, and . The first return reverses the chosen stress-pulse polarity; the second interface produces no normal-incidence P return.
For a particle-velocity amplitude convention, and , giving and respectively. These are amplitude coefficients, not fractions of energy. The lossless reflected and transmitted energy fractions are and , which sum to one.