Research Article

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

Figure 11

3D distribution of TOCo of the A shale bed (a) and the B shale bed (b) in the study area (×20 vertical exaggeration). Relatively high TOCo distribution in the A bed is shown at the upper layer and northwestern region and in the B bed is shown at the lower layer and southern region.
(a)
(b)