English: Ocean medium-grained turbidite family for sand and sand–mud turbidites
The ideal Bouma facies model showing the complete sequence of divisions A–E (Bouma et al, 1962), and typical partial sequences found commonly in nature, is given. F is now commonly used for pelagites above a turbidite.
Bouma, A.H. Sedimentology of Some Flysch Deposits; A Graphic Approach to Facies Interpretation; Elsevier: Amsterdam, The Netherlands, 1962.
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