Petrography and geochemistry of the Mesoarchean Bikoula banded iron formation in the Ntem complex (Congo craton), Southern Cameroon: Implications for its origin
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The Bikoula BIF has undergone granulite-facies metamorphism.

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The primary chemical protolith was contaminated by clastic material.

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Basin waters were influenced by high-temperature hydrothermal fluids.

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Deposition occurred in a basin that was at least partly anoxic or suboxic.

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