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. 2019 Jul 17;25:104267. doi: 10.1016/j.dib.2019.104267

Fig. 4.

Fig. 4

Site Bol'shaya Balaknya 16. (A) The 35 m high river-cut cliff at BBR 16 (Fig. 1; sediment log is Fig. 9 in [1]). Undeformed unit A fluvial sediments are indicated, over which is ∼15 m of glaciotectonically deformed fluvial and marine sediment. (B) Bar cross-laminated sand (unit A), deposited in a shallow marine setting. (C) Climbing type-B ripple lamination, Sr(B), with silt draping, on top of which is sand with planar parallel-lamination and massive, normally graded sand (unit A), deposited in a shallow marine setting. The arrow indicates an interbedded ripple form set. (D–E) Stacked successions of interbedded ripple-laminated sand, Sr(A), often with draping silt, and massive, normally graded sand beds (unit A), deposited in a shallow marine setting. (F) Undeformed ripple-laminated sand (unit A), which above a decollement surface (red arrows) are strongly deformed with a stress transfer from SE. (G) Marine clay (unit B). (H). At ∼38–39 m; unit C diamict with a prominent sand wedge (unit D), that is aeolian sediment infill into a polygonal frost wedge. (I) Large-scale tectonics into unit A sediment (∼31 m).