Compositional Trends Among IID Irons; Their Possible Formation from the P-rich Lower Magma in a Two-Layer Core

Details Compositional Trends Among IID Irons; Their Possible Formation from the P-rich Lower Magma in a Two-Layer Core Compositional Trends Among IID Irons; Their Possible Formation from the P-rich Lower Magma in a Two-Layer Core

Mar 2006

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2006lpi....37.2119w&link_type=abstract

37th Annual Lunar and Planetary Science Conference, March 13-17, 2006, League City, Texas, abstract no.2119

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Scientific paper

Magmatic iron-meteorite group IID has a low S content but high contents
of other volatiles. We suggest that the S was extracted in an early
metallic magma. A second metallic magma formed at much
higher-temperatures was parental to the IID irons.

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