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LaTeX Math Inline
bodyx
 is a lateral offset between the seismic source and  and seismic receiver,

LaTeX Math Inline
bodyl(x,y,z)
 – trajectory of reflection wave from seismic source @ source @ 
LaTeX Math Inline
body(x = 0, \, y = 0, \, z = 0)
 and seismic receiver @ receiver @ 
LaTeX Math Inline
body(x, \, y = 0, \, z = 0)

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LaTeX Math Inline
bodyV_{rms}
 – average p-wave velocity through the reflecting travel distance  between the seismic source and  and seismic sensorreceiver:

LaTeX Math Block
alignmentleft
V^2_{rms} = \frac{\sum_i^N  V_p^2(t_i) \, \delta t_i}{\sum_i^N \delta t_i}= \frac{\sum_i^N  V_p(t_i) \, \delta h_i}{\sum_i^N \frac{\delta h_i}{V_p(t_i)}}

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