Redistribution of Georgia tektites as channel lag deposits

Physics

Scientific paper

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Tektites, Mineral Deposits, Geochemistry, Georgia, Rivers

Scientific paper

It is suggested that the georgiaites of the Altamaha Formation were
deposited as channel lag. Continuous migration of a river channel
furnishes a constant source of lag material, including tektites, as the
river erodes its banks in the tektite source area.

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