CMPAnalysis | R Documentation |
Transform the space-time domain of the radargram into a velocity-time domain to obtain the velocity spectrum (i.e. change in wave velocity with depth or time). This is achieved by applying Normal Move-Out (NMO) corrections to the radargram for the range of selected velocities and computing a coherency measure for each result. In RGPR, the coherency measure can be defined using different functions: "semblance", "winsemblance", "wincoherence", "wincoherence2".
## S4 method for signature 'GPR'
CMPAnalysis(
x,
method = c("semblance", "winsemblance", "wincoherence", "wincoherence2"),
v = NULL,
w = NULL
)
x |
An object of the class |
method |
A length-one character vector |
v |
A numeric vector defining at which velocities the analysis is performed |
w |
A length-one numeric vector defining the window length for the methods 'wincoherence' and 'wincoherence2'. |
either use 'rec' and 'trans' to compute the distance between the antennas or give the distance between the antennas (asep) or seq(x@antsep, by = x@dx, length.out = length(x))
also described as the ratio of input to output energy (Niedell and Taner, 1971)
windowed semblance
Windowed coherence measure based on eigen-decomposition that estimates the signal-to-noise ratio for high resolution velocity analysis (Sacchi, 2002)
Windowed coherence measure based on a log-generalized likelihood ratio which tests the hypothesis of equality of eigenvalues (Key and Smithson, 1990)
Neidell and Taner (1971) Semblance and other coherency measures for multichannel data. Geophysics, 36(3):482-497.
Key and Smithson (1990) New approach to seismic-reflection event detection and velocity determination. Geophysics, 55(8):1057-1069.
Textbook: Sacchi (2002) Statistical and Transform Methods in Geophysical Signal Processing
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