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- W1973060571 abstract "Based on a knowledge of the Bristol Channel hydrography, the quantitative heavy mineral distribution, and the individual mineral threshold values, a model for equivalence/inequivalence values and heavy mineral enrichment is presented. Hydraulic inequivalence in the Channel is a result of (I) preferential mineral size from the source; this controls the mineral suite changes created by (2) differential entrainment of minerals by density and size. Differential mineral transport of heavy minerals depends upon the hydraulic conditions of unidirectional and oscillatory flow, separately and in combination, acting on a seabed of certain roughness. Such a model can be used to explain the development of heavy mineral enrichment found on the open (high energy) beaches and in the areas of local tidal current enhancement." @default.
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- W1973060571 date "1981-05-01" @default.
- W1973060571 modified "2023-09-27" @default.
- W1973060571 title "Hydrodynamic factors controlling the distribution of heavy minerals (Bristol Channel)" @default.
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- W1973060571 doi "https://doi.org/10.1016/s0302-3524(81)80086-2" @default.
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