Archaean asteroid impacts, banded iron formations and MIF-S anomalies: A discussion

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Glikson, Andrew

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Academic Press

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The origin of mass-independent fractionation (MIF-S) of sulphur isotopes (δ33S) recorded in sediments older than 2.45 Ga is widely interpreted in terms of UV-triggered reactions under oxygen-poor ozone-depleted atmosphere conditions (Farquhar, J., Bao, H

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Icarus

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Restricted until

2037-12-31