Fig. 2From: The turbidite-contourite-tidalite-baroclinite-hybridite problem: orthodoxy vs. empirical evidence behind the “Bouma Sequence”The first turbidite-fan link proposed by Bouma (1962). a The turbidite facies model with five internal divisions (Ta, Tb, Tc, Td, and Te). This vertical facies model is commonly known as “the Bouma Sequence.”; b Areal distribution of turbidite facies in a submarine fan (after Bouma 1962; after Shanmugam 2016a, b)Back to article page