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Banded Iron Formation

Banded Iron Formation. Banded iron formation or BIF is a chemical sediment typically thin-bedded or laminated with 15 iron of sedimentary origin Figure 8.6. BIF has a very distinct distribution with time Figure 8.25. It is found in minor amounts in the early Archean and in large amounts in the late Archean appears again around 1.85 Ga

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