A size control for quartz silt (making particulates at planetary surfaces) |
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Authors: | Ian Smalley Claudio Vita-Finzi |
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Institution: | 1. Giotto Loess Research Group, Arkwright Materials Project, Nottingham Trent University, Nottingham, NG1 4BU, UK 2. Mineralogy Department, Natural History Museum, London, SW7 5BD, UK
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Abstract: | Quartz silt is widespread in terrestrial sediments 1]. Its ubiquity has led to its neglect as a geomaterial, and studies of silt as such are relatively rare, but it presents an interesting and continuing petrological problem. Is silt a specific geological material, is it defined by a formation process, and a set of size parameters? In the world of clastic quartz sedimentology there are obvious mode sizes; there is a sand mode at around 300–500 μm and a silt mode, an order of magnitude smaller, at 30–50 μm. Are these both defined by specific geological processes? |
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