Native Iron in the Chaibasa Shales: Result of a Pre 1.6 Ga Impact?

Physics

Scientific paper

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Scientific paper

We have found bulbous droplets and broken fragments of native Fe in the
pre-1.6 Ga Chaibasa shales. The native Fe is primary and is not
detrital. We infer that the native Fe grains must have come from melting
and reduction of Fe rich material during a nearby impact event.

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