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説明
Abstract A quantitative model for the settling of a spherical body in a Newtonian fluid is developed and is applied to the distribution of phenocrystic olivine in a differentiated dolerite sill. Satisfactory agreement was obtained between the model calculation and the observed modal olivine distribution in the sill.
収録刊行物
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- Lithos
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Lithos 7 (3), 133-137, 1974-01
Elsevier BV
