--> Well-bedded successions of thin claystone, siltstone an very fine sandstones.

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Figure 2. Well-bedded successions of thin claystone, siltstone an very fine sandstones. The claystone are dominant at the base of sequence while the sandstones and siltstone are dominant at the top of the sequence. This facies was deposited by traction and fallout from turbidity flows. This facies is known as classic turbidites.