Visualize and interpret the geometry, heterogeneity and lateral ...

On the western side of the island one can clearly see that the sandy unit has a pinch outtowards SE (Figure 4.2 H and I), indicating a possible channel feature. The sandstonecontinues on the other side of the fault on both sides of the island and has a maximumthickness of around 15 meters (Figure 4.1 and Figure 4.2). On this part of the island thestratigraphic unit of Channel body 2 is approximately 30 meters above Channel body 1(Figure 4.1 and Figure 4.2). One can also see that the sand units look similar in colour.Figure 4.3: This figure illustrates Binnedalen with its associated log. (A) A illustration ofthe log taken of Binnedalen. (B) An overview photo of Binnedalen. The right part of thisphoto is of the same area as the left part of picture 4.4. (C) Zooming in on Channel body2, with the interpretation of the pinch out seen to the left of the picture.34