Estimation of Generated and Retained Gas Volume of the Besa River Formation in Liard Basin through 3-Dimensional Static Geochemical Modeling

Figure 6

Correlation between calculated GOCpd and measured TOCpd of A-038-B/094-N-08 [17] and A-068-D/094-O-05 [18], and B-023-K/094-O-05 [19] and B-D003-K/094-O-12 [19] GOCpd shows a relatively very small weight percent (wt%) compared to TOCpd and is less than 1 wt% in four boreholes.