Explore: Amplitude Variation With Offset Analysis

In geophysics and reflection seismology, amplitude versus offset (AVO) or amplitude variation with offset is the general term for referring to the dependency

is the amplitude, ω is the angular frequency, usually given in degrees per hour, corresponding to t measured in hours, p is the phase offset with regard

affecting the amplitude of a returning seismic wave when the angle of incidence is altered — also known as amplitude versus offset analysis — which is a

resonant frequency slightly offset from the carrier. As the frequency rises and falls the tuned circuit provides a changing amplitude of response, converting

2017). "A high-resolution weighted AB semblance for dealing with amplitude-variation-with-offset phenomenon". Geophysics. 82 (2): V85–V93. Bibcode:2017Geop

the classical analysis, all of the other information that might theoretically be obtained by detailed analysis of the intensity variations in an interferogram

sounds — variations of pressure in air or other media. In these cases, the waveform is an attribute that is independent of the frequency, amplitude, or phase

company specializing in anisotropic processing (AZIM), AVO (amplitude variation with offset) analysis, and azimuthal velocity modeling. 2004 – Concept Systems

When interfering, two waves add together to create a wave of greater amplitude than either one (constructive interference) or subtract from each other

offset current, and even with matched resistances a small offset voltage (distinct from the input offset voltage below) can be produced. This offset voltage