GLOSSARY

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T^2_x = T^2_0 + \frac{4 x^2}{V^2_{rms}}

where where

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

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where 

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bodyH
 is the depth of the reflecting boundary, 

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

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