![Zabriskie Quartzite, Eagle Mountain, California In well-cemented, very pure quartz arenites like this, planar lamination can be difficult to detect. Here. - ppt download Zabriskie Quartzite, Eagle Mountain, California In well-cemented, very pure quartz arenites like this, planar lamination can be difficult to detect. Here. - ppt download](https://images.slideplayer.com/32/10010443/slides/slide_3.jpg)
Zabriskie Quartzite, Eagle Mountain, California In well-cemented, very pure quartz arenites like this, planar lamination can be difficult to detect. Here. - ppt download
![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
Horizontal planar bedding. A= Horizontal planar bedding (lamination) in... | Download Scientific Diagram
![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 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](https://media.springernature.com/lw685/springer-static/image/art%3A10.1007%2Fs12182-020-00534-x/MediaObjects/12182_2020_534_Fig7_HTML.png)
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
![Distal turbidite fan/lobe succession of the Late Oligocene Zuberec Fm. – architecture and hierarchy (Central Western Carpathians, Orava–Podhale basin) Distal turbidite fan/lobe succession of the Late Oligocene Zuberec Fm. – architecture and hierarchy (Central Western Carpathians, Orava–Podhale basin)](https://www.degruyter.com/document/doi/10.1515/geo-2017-0030/asset/graphic/j_geo-2017-0030_fig_003.jpg)
Distal turbidite fan/lobe succession of the Late Oligocene Zuberec Fm. – architecture and hierarchy (Central Western Carpathians, Orava–Podhale basin)
![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.
![Sedimentary facies of the upper Cambrian (Furongian; Jiangshanian and Sunwaptan) Tunnel City Group, Upper Mississippi Valley: New insight on the old stormy debate - ScienceDirect Sedimentary facies of the upper Cambrian (Furongian; Jiangshanian and Sunwaptan) Tunnel City Group, Upper Mississippi Valley: New insight on the old stormy debate - ScienceDirect](https://ars.els-cdn.com/content/image/1-s2.0-S0037073813001814-gr6.jpg)
Sedimentary facies of the upper Cambrian (Furongian; Jiangshanian and Sunwaptan) Tunnel City Group, Upper Mississippi Valley: New insight on the old stormy debate - ScienceDirect
![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/775c705484476c8cce90c5e6bdb348cae5dadbb1/3-Figure2-1.png)
PDF] Upper-regime parallel lamination as the result of turbulent sediment transport and low-amplitude bed forms | Semantic Scholar
![Planar and trough cross-stratification and horizontal lamination in... | Download Scientific Diagram Planar and trough cross-stratification and horizontal lamination in... | Download Scientific Diagram](https://www.researchgate.net/profile/P-Worsley/publication/285633879/figure/fig5/AS:669459391975452@1536622965721/Planar-and-trough-cross-stratification-and-horizontal-lamination-in-alluvial-sands.png)