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- W4310209554 abstract "This is a dataset of grain-size distribution in sub- and supercritical flow sediments of a Gilbert-type delta from an outcrop in North Germany. Thirteen samples of ca 2.5 kg were dried (at 105°C), and homogenised twice with a sample divider. A representative sample of 1-2 g was then analysed using laser diffraction. The grain-size distribution of the sand has a maximum between fine to medium sand, with a long fine fraction tail down to 0.06 µm and occasional coarse fractions (up to 1.5 mm) in some samples. Specific grain-size distributions correlate with the different sedimentary bedforms from which the samples were taken. This data is important for two reasons: Firstly, sedimentary structures formed by Froude supercritical flows are controlled by grain-size. However, few studies have provided grain-size datasets from the natural record, which often have a much wider grain-size distribution than experimentally-produced supercritical flow deposits. Secondly, the sands were deformed subsequently by disaggregation bands, a type of geological fault that only develops in porous granular materials, i.e. well-sorted, medium sand. The disaggregation bands are indicative of seismic or even aseismic, creeping movement of basement faults." @default.
- W4310209554 created "2022-11-30" @default.
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- W4310209554 date "2023-02-01" @default.
- W4310209554 modified "2023-09-26" @default.
- W4310209554 title "Grain-size distribution dataset of supercritical flow sediments from a Gilbert-type delta that are associated with disaggregation bands" @default.
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- W4310209554 doi "https://doi.org/10.1016/j.dib.2022.108792" @default.
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