Detrital magnetite and chromite in Jack Hills quartzite cobbles: Further evidence for the preservation of primary magnetizations and new insights into sediment provenance
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Two labs report magnetizations surviving peak metamorphism in Jack Hills sediments.

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These data support zircon magnetizations as records of a Hadean geodynamo.

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Cr–Fe spinels suggest a layered intrusive source distinct from that of the zircons.

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