Estimation of Generated and Retained Gas Volume of the Besa River Formation in Liard Basin through 3-Dimensional Static Geochemical Modeling
Figure 7
Correlation between calculated NGOCpd and 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]. These boreholes have considerably high coefficient of determinations. The NGOCpd can be alternative to TOCpd in Equation (2).
