📄 grm.par.main
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GRM - Generalized Reciprocal refraction analysis for a single layer grm <stdin >stdout [parameters] Required parameters: nt= Number of arrival time pairs dx= Geophone spacing (m) v0= Velocity in weathering layer (m/s) abtime= If set to 0, use last time as a-b, else give time (ms) Optional parameters: XY= Value of XY if you want to override the optimum XY algorithm in the program. If it is not an integer multiple of dx, then it will be converted to the closest one. XYmax Maximum offset distance allowed when searching for optimum XY (m) (Default is 2*dx*10) depthres Size of increment in x during verical depth search(m) (Default is 0.5m) Input file: 4 column ASCII - x,y, forward time, reverse time Output file: 1) XYoptimum 2) apparent refractor velcocity 3) x, y, z(x,y), y-z(x,y) z(x,y) = calculated (GRM) depth below (x y) y-z(x,y) = GRM depth subtracted from y - absolute depth ............. 4) x, y, d(x,y), y-d(x,y), (error) d(x,y) = dip corrected depth estimate below (x,y) y-d(x,y) = dip corrected absolute depth error = estimated error in depth due only to the inexact matching of tangents to arcs in dip estimate. If the XY calculation is bypassed and XY specified, the values used will precede 1) above. XYoptimum will still be calculated and displayed for reference. Notes: Uses average refactor velocity along interface. Credits: CWP: Steven D. Sheaffer D. Palmer, "The Generalized Reciprocal Method of Seismic Refraction Interpretation", SEG, 1982.
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