GLOSSARY

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LaTeX Math Inline
bodyT^2_0
 is reflection time at zero offset (which means the normal incident wave reflection):

LaTeX Math Block
alignmentleft
T_0 = 2 \cdot \int_0^H \ \frac{\delta z}{V_p(z)}

where 

LaTeX Math Inline
bodyH
 is the depth of the reflecting boundary,

 

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

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