Distribution of K-Ar age marks in Pacific bottom sediments is shown on the base of large analytical material. Dependence of K-Ar age marks on abundance of potassium-bearing authigenic diagenetic minerals (glauconite, phillipsite) widely spread in the studied part of the World Oceans.
Supplement to: Krylov, AYa; Lisitzina, Nadezhda A; Mazina, TI; Silin, YuI; Tsovbun, YaM (1984): Age marks of muds from the North Pacific. Litologiya i Poleznyye Iskopaemyye (Lithology and Mineral Resources), 19(2), 23-37