Isotopic evolution of planetary crusts by hypervelocity impacts evidenced by Fe in microtektites.

Nat Commun · 2021 · PMC8458397 · PMID 34552090

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only marginally significantno p-value reported

The δ 56/54 Fe values and FeO concentrations in microtektites, found in ODP sediment cores drilled in the South China and the Sulu Seas indicate only marginally significant Fe isotope ratio variability.

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