Changes

Jump to navigation Jump to search
Line 52: Line 52:  
Convert time to depth by multiplying the time structure map and the depth conversion velocity map, i.e.,
 
Convert time to depth by multiplying the time structure map and the depth conversion velocity map, i.e.,
   −
:<math>z(x,y) = \frac{\upsilon(x,y)*t(x,y)}{2}</math>
+
:<math>z(x,y) = \frac{\upsilon(x,y) \times t(x,y)}{2}</math>
    
The factor of one-half is necessary because the times are two-way vertical times and we only want the one-way depth. [[:file:interpreting-seismic-data_fig12-14.png|Figure 3]] shows the process and result for the Glenn Pool Wilcox horizon.
 
The factor of one-half is necessary because the times are two-way vertical times and we only want the one-way depth. [[:file:interpreting-seismic-data_fig12-14.png|Figure 3]] shows the process and result for the Glenn Pool Wilcox horizon.

Navigation menu