The origin of planar lamination in fine‐grained sediment deposited by subaqueous sediment gravity flows
Abstract Planar lamination is a ubiquitous component of modern and ancient fine‐grained sediments deposited by subaqueous sediment gravity flows. These sediments commonly exhibit alternating sub‐millimetre‐thick, sharply bounded silt‐rich and clay‐rich layers that change little in thickness or sedim...
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| 主要な著者: | , |
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| フォーマット: | Artigo |
| 言語: | Inglês |
| 出版事項: |
Wiley
2024-11-01
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| シリーズ: | The Depositional Record |
| 主題: | |
| オンライン･アクセス: | https://doi.org/10.1002/dep2.257 |
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