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Architecture and morphodynamics of subcritical sediment waves in an ancient channel–lobe transition zone - Hofstra - 2018 - Sedimentology - Wiley Online Library
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PDF] Upper-regime parallel lamination as the result of turbulent sediment transport and low-amplitude bed forms | Semantic Scholar
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Planar and trough cross-stratification and horizontal lamination in... | Download Scientific Diagram
![Figure F74. Comparison of sedimentary structures visible on a core photograph compared to a CT scan viewed from a different angle. A. Core photograph. Planar, wavy, and cross lamination. B. CT scan. Figure F74. Comparison of sedimentary structures visible on a core photograph compared to a CT scan viewed from a different angle. A. Core photograph. Planar, wavy, and cross lamination. B. CT scan.](http://www-odp.tamu.edu/publications/210_IR/chap_03/images/03_f74.jpg)
Figure F74. Comparison of sedimentary structures visible on a core photograph compared to a CT scan viewed from a different angle. A. Core photograph. Planar, wavy, and cross lamination. B. CT scan.
![PDF] Upper-regime parallel lamination as the result of turbulent sediment transport and low-amplitude bed forms | Semantic Scholar PDF] Upper-regime parallel lamination as the result of turbulent sediment transport and low-amplitude bed forms | Semantic Scholar](https://d3i71xaburhd42.cloudfront.net/775c705484476c8cce90c5e6bdb348cae5dadbb1/2-Figure1-1.png)
PDF] Upper-regime parallel lamination as the result of turbulent sediment transport and low-amplitude bed forms | Semantic Scholar
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Bed type and flow mechanism of deep water sub-lacustrine fan fringe facies: an example from the Middle Permian Lucaogou Formation in Southern Junggar Basin of NW China | SpringerLink
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Distal turbidite fan/lobe succession of the Late Oligocene Zuberec Fm. – architecture and hierarchy (Central Western Carpathians, Orava–Podhale basin)
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