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The Bouma sequence (named after Arnold H. Bouma , 1932–2011) describes a classic set of sedimentary structures in turbidite beds deposited by turbidity currents at the bottoms of lakes, oceans and rivers.
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bouma deposited flow energy grains structures layer sequence layers settle current turbidite flows turbidity top often base move currents also
| Subject | Predicate | Object | Confidence | Src |
|---|---|---|---|---|
| groove casts | instance of | The current energy is such that sole marks | 0.80 | text |
| flute casts | instance of | The current energy is such that sole marks | 0.80 | text |
| parting lineation can form on top the bed beneath the flow | instance of | The current energy is such that sole marks | 0.80 | text |
| and be preserved as molds | instance of | The current energy is such that sole marks | 0.80 | text |
| casts on the underside of the Bouma B layer.Bouma A is the first layer deposited by a flow | instance of | The current energy is such that sole marks | 0.80 | text |
| provided the flow has sufficient energy | instance of | The current energy is such that sole marks | 0.80 | text |
| Bouma sequence | related to Description | The Bouma | 0.60 | section |
| Bouma sequence | related to Description | An | 0.60 | section |
| Bouma sequence | related to Description | Lowe | 0.60 | section |
| Bouma sequence | related to Description | Each | 0.60 | section |
| Bouma sequence | related to Description | Bouma | 0.60 | section |
| Bouma sequence | related to Description | Most | 0.60 | section |
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