Post-LGM changes of sedimentary environments and bottom-current activity recorded in shallow-water contourite drifts of the Hupo Basin, East Sea (Sea of Japan)
Shallow-water contourite drifts preserve detailed records of the interplay between waves, currents, and sea-level changes; however, their formative processes remain less constrained than those of deep-water contourites. Here, we examine the post–Last Glacial Maximum (LGM) sedimentary environments and bottom-current a...