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 526

S HS : hummocky-stratified sandstone

S SS : swaley-stratified sandstone

S PS : planar parallel-stratified sandstone

(A)

vf fm cvc vf fmcvc vf fmcvc

vf fmcvc

silt
sand

silt
sand

silt
sand

silt
sand

Facies associations: A B C

Tidal ridge deposits Inter-ridge deposits Wave-worked deposits

Fig. 7. Example intervals of core logs showing the three main facies associations of the Garn Fm. in Kristin Field. The log
portions are from: (A) well 6406/2-R-4H, depth 5216.80 to 5227.25 m; (B) well 6506/11-6, depth 4736.50 to 4747.95 m;
(C) well 6406/2-5 AT2, depth 5392.30 to 5403.75 m; and (D) well 6506/11-6, depth 4659.30 to 4670.75 m.