1954
DOI: 10.1086/626206
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Relationships of Plasticity and Grain Size of Lake Agassiz Sediments

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“…The grain diameter is shown in φ scale as φ=−log 2 d, where d represents the diameter. The definition of the sorting is from Rominger (1954): very well sorted (0b σφ b 1), well sorted (1b σφb 2), normally sorted (2 b σφ b 3), poorly sorted (3b σφb 4), and very poorly sorted (4 b σφ). Grain size distributions in the SWRC (loc.…”
Section: Grain Size Analysismentioning
confidence: 99%
“…The grain diameter is shown in φ scale as φ=−log 2 d, where d represents the diameter. The definition of the sorting is from Rominger (1954): very well sorted (0b σφ b 1), well sorted (1b σφb 2), normally sorted (2 b σφ b 3), poorly sorted (3b σφb 4), and very poorly sorted (4 b σφ). Grain size distributions in the SWRC (loc.…”
Section: Grain Size Analysismentioning
confidence: 99%