Iron transport in chondrites: evidence from the Warrenton meteorite

Details Iron transport in chondrites: evidence from the Warrenton meteorite Iron transport in chondrites: evidence from the Warrenton meteorite

Aug 1972

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1972gecoa..36..913k&link_type=abstract

Geochimica et Cosmochimica Acta, vol. 36, Issue 8, pp.913-914

Physics

3

Scientific paper

Veins of iron enrichment in an olivine chondrule in Warrenton are
attributed to migration of iron prior to final consolidation. Aqueous
transport along cracks is suggested as the most plausible mechanism
responsible for such migration, with possible implications for
`metamorphic' theories of iron distribution in chondrites.

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