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Summary
| Description |
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.
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| Date | |
| Source | [1] doi:10.3390/geosciences10020068 |
| Author | Dorrik Stow and Zeinab Smillie |
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 22:23, 24 November 2021 | 3,764 × 2,062 (1.29 MB) | Epipelagic | Uploaded a work by Dorrik Stow and Zeinab Smillie from [https://www.mdpi.com/2076-3263/10/2/68/htm] {{doi|10.3390/geosciences10020068}} with UploadWizard |
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