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

<div>Isopach maps of the A shale bed (a) and the B shale bed (b). Thickness tends to increase toward the north, and relatively, the B bed is thicker than the A bed.</div>

Geofluids

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Figure 5

Figure 5: Estimation of Generated and Retained Gas Volume of the Besa River Formation in Liard Basin through 3-Dimensional Static Geochemical Modeling 

Figure 5 | Estimation of Generated and Retained Gas Volume of the Besa River Formation in Liard Basin through 3-Dimensional Static Geochemical Modeling 