My questions are about the calculation of Site Fundamental Frequency using Horizontal to Vertical Spectral Ratio (HVSR) based on the Fourier amplitude spectrum:
As the distance from the source of the earthquake increases, the difference between the acceleration of the horizontal and vertical components becomes very large, and by dividing these two values, no matter how large the horizontal component is, when divided by the vertical component, its effect is very small. How can this effect be explained?