Research Article

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

Figure 8

Correlation between calculated TOCpd (Schmoker_TOCpd) 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]. Coefficients of determinations are from 0.540 to 0.753; these value means that the Schmoker_TOCpd has a substitute instead of measured TOCpd in boreholes without geochemical data.