Melt solidification and late-stage evaporation in the evolution of a FUN inclusion from the Vigarano C3V chondrite

Details Melt solidification and late-stage evaporation in the evolution of a FUN inclusion from the Vigarano C3V chondrite Melt solidification and late-stage evaporation in the evolution of a FUN inclusion from the Vigarano C3V chondrite

Feb 1991

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1991gecoa..55..621d&link_type=abstract

Geochimica et Cosmochimica Acta (ISSN 0016-7037), vol. 55, Feb. 1991, p. 621-637.

Mathematics

Logic

27

Carbonaceous Chondrites, Inclusions, Isotope Separation, Olivine, Petrology, Spinel, Crystallization, Evaporation, Microstructure, Solidification, Meteorites, Melt, Evaporation, Evolution, Inclusions, Volatilization, Vigarano, Chondrites, Cv3 Chondrites, C Chondrites, Refractory Material, Carbonaceous Chondrites, Description, Stony Meteorites, Samples, Meteorite, Compositon, Mantle, Core, Origin, Formation, Procedure, Mineralogy, Laboratory Studies, Petrology, Chemistry, Isotopes, Electron Microscopy, Sem,

Scientific paper

Results are presented on a detailed petrologic, chemical, and isotopic study of the so-called FUN inclusion (1623-5) from the Vigarano C3V chondrite. It is shown that the precursor material from which the Vigarano 1623-5 has formed contained some nuclear isotopic anomalies; this precursor was composed of melted and crystallized spinel, olivine, fassaite, and melilite. The results on the petrologic and isotopic properties of 1623-5 indicate unambiguously the action of volatilization in the evolution of this inclusion.

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