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The paper discusses results of sedimentological, faunal (molluscs, ostracods) and geochemical studies of an 80-cm-thick rhythmite succession within a glaciolacustrine sequence (8–10m in thickness) of the Ławki Formation exposed at the Parchliny C site, in the tectonically active Kleszczów Graben, central Poland. Sedimentological studies show the predominance of rhythmically deposited pale grey muds...
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