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Three modes of entry of solid phases from the lands to the seas are considered: by glaciers, by rivers and by atmospheric winds. The compositions of the clay size fraction are also related to rates of accumulation of the non-biogenous phases.","descriptionType":"Abstract"},{"description":"size fraction \u0026lt;2µm, value \u0026lt;1 means traces","descriptionType":"TechnicalInfo"},{"description":"Supplement to: Griffin, John J; Windom, Herbert; Goldberg, Edward D (1968): The distribution of clay minerals in the World Ocean. Deep-Sea Research and Oceanographic Abstracts, 15(4), 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