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

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4.2.2 Channel body 6 <strong>and</strong> 7 (Western side of Lyngefjellet)Channel body 6 shown on Figure 4.13 has a maximum thickness of 11 meters <strong>and</strong> is around210 meters wide. While Channel body 7 (Figure 4.13) is 6 meters thick <strong>and</strong> 145 meters wide.These two channels are described in <strong>the</strong> same subsection partly because <strong>the</strong>y are situated in<strong>the</strong> same area, but also because <strong>the</strong>ir <strong>geometry</strong> is similar. Channel body 6 is situated 29meters below Hopen member, while Channel body 7 is situated around 50 meters belowHopen member.Channel body 6 <strong>and</strong> 7 seem to have a higher portion of mud on <strong>the</strong> left side of <strong>the</strong> channelbodies, than on <strong>the</strong> right side (Figure 4.13). The colour also changes from light orange on <strong>the</strong>right side to more grey/black colour on <strong>the</strong> left side. It also seems to be finer material towards<strong>the</strong> top of <strong>the</strong> channel bodies (Figure 4.13). The channel bodies consist of several dippinglayers (Figure 4.13).By taking a closer look at Channel body 6, it seems like <strong>the</strong> layers at its sou<strong>the</strong>rn most partappear to pinch out towards <strong>the</strong> overlying s<strong>and</strong>stone unit (Figure 4.13).On Channel body 7 it is difficult to see any clear indications of dipping layers towards <strong>the</strong>north of <strong>the</strong> channel body, while on <strong>the</strong> sou<strong>the</strong>rn side <strong>the</strong> dipping layers are clear (Figure4.13).(1) DiscussionThe dipping layers which seem to pinch out towards <strong>the</strong> overlying s<strong>and</strong>stone unit can indicatepresence of amalgamating channel bodies, which would mean that <strong>the</strong> channel body actuallyconsists of at least two channels, where <strong>the</strong> youngest erode into <strong>the</strong> underlying channel. Thiscan contribute to an <strong>interpret</strong>ation of Channel body 6, as a channel body consisting of ayounger channel with point bars <strong>and</strong> channel infill, possibly mud-plug, while <strong>the</strong> oldestchannel only displays its point bars. This indicates a multi<strong>lateral</strong> channel body, which isdefined as <strong>lateral</strong>ly coalescent s<strong>and</strong> bodies (Potter, 1967; Gibling, 2006).Channel body 7 seems to be single-story where <strong>the</strong> dipping layers to <strong>the</strong> south are point bars<strong>and</strong> <strong>the</strong> area marked with red in Figure 4.13 is channel infill, possibly mud-plugs.52

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