Environmental Engineering Reference
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FIGURE 8 Example of a dynamic FMI Image (Schlumberger tool) from a Campanian deep-sea
fan system of the Vøring Basin, Norwegian Sea (cf. Knaust, 2009a ). Bright color (resistive) corre-
sponds to sandstone and dark color (conductive) to mudstone. The 2-m thick interval is accompanied
by four representative core image examples (about 10 cm wide) taken from the corresponding
slabbed core to illustrate the lithological changes, the bioturbation index (BI), and recognizable trace
fossils. Note the muddy, meniscate backfill of cf. Ophiomorpha isp. that is also detectable in the
sandy portions of the borehole image (e.g., at 3115.7 and 3115.1 m). The nodules at 3116.1 m con-
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