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Examples
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Varved, lacustrine clays overlain by fluvial sands and peat deposits are common.
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Varved clay chronology has shown that the annual withdrawal of the ice margin was fast, up to 200-500 m per year, leaving the regular ridges of till which reflect the probable positions of the intermittently retreating margin of ice.
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A 5000-yr Record of Climate Change in Varved Sediments from the Oxygen Minimum Zone off Pakistan, Northeastern Arabian Sea, Quaternary Research 51, 39″â¬Å53 1999
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