Three lithofacies assemblages of upper slope, lower slope and submarinefan emerged in the slope.
在这个斜坡背景中出现了上斜坡相、下斜坡相与 海底 扇相等3种类型的岩相组合。
2
It is considered that F4 layer is a submarinefan generated by gravity flow in marine environment, with a regressive-transgressive sequence from the lower to the upper parts.