To get insight into the seismic reflection behavior, which is considered the basis of seismic imaging.
The program calculates the amplitude of the four seismic waves generated when reaching an interface with impedance mismatch. Alpha and beta are the p-velocity and s-velocity, respectively and rho is the density. Clicking on the canvas will reset the graphs. Moving the mouse in the area of the incident wave will change the incident angle. The length of the 4 reflected/transmitted vectors are proportional to their amplitudes.