Low-temperature exsolution in refractory siderophile element-rich opaque assemblages from the Leoville carbonaceous chondrite

Details Low-temperature exsolution in refractory siderophile element-rich opaque assemblages from the Leoville carbonaceous chondrite Low-temperature exsolution in refractory siderophile element-rich opaque assemblages from the Leoville carbonaceous chondrite

May 1992

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1992e%26psl.110...67s&link_type=abstract

Earth and Planetary Science Letters (ISSN 0012-821X), vol. 110, no. 1-4, May 1992, p. 67-75.

Computer Science

Carbonaceous Chondrites, Crystallography, Meteoritic Composition, Crystallization, Inclusions, Phase Diagrams

Scientific paper

The discovery is reported of opaque assemblages in the Leoville carbonaceous chondrite with both clear textural and chemical evidence of a major role for resolution and equilibration at relatively low temperatures in the formation of refractory siderophile element-rich assemblages. The observed phase compositions are used to bracket a previously inferred phase boundary in the Fe-Ni-Ru system. The first meteoritic occurrence of goldmanite is also reported.

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