The Garn Formation (Bajocian-Bathonian) in the Kristin Field, Halten Terrace: its origin, facies architecture and primary heterogeneity model - From Depositional Systems to Sedimentary Successions on the Norwegian Continental Margin - page 523

(A) (B) (C) (D) (E)

S PS

Fig. 6. Core intervals showing sedimentary facies of the Garn Fm., Kristin Field. The facies letter code is as in Table 1 and
in the text; other symbols: RS − reactivation surface; MD − mud drape; BFR − backflow ripples; B − burrows. For the location
of wells, see Fig. 4. The cores samples are from: (A) well 6506/11-6, depth 4763 − 4764 m; (B) well 6506/11-6, depth 4762
to 4763 m; (C) well 6506/11-6, depth 4743 to 4744 m; (D) well 6506/11-6, depth 4742 to 4743 m; (E) well 6506/11-6, depth
4741 to 4742 m;