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Carbon in glass inclusions in the Allende meteorite
Author(s) -
Makjanic J.,
Touret J. L. R.,
Vis R. D.,
Verheul H.
Publication year - 1989
Publication title -
meteoritics
Language(s) - English
Resource type - Journals
eISSN - 1945-5100
pISSN - 0026-1114
DOI - 10.1111/j.1945-5100.1989.tb00941.x
Subject(s) - allende meteorite , melt inclusions , electron microprobe , chondrule , graphite , meteorite , fluid inclusions , mineralogy , olivine , microprobe , inclusion (mineral) , chondrite , carbonaceous chondrite , carbon fibers , silicate , analytical chemistry (journal) , parent body , geology , materials science , chemistry , astrobiology , composite material , quartz , physics , organic chemistry , chromatography , composite number
— Olivines in chondrules of the Allende CV3 carbonaceous chondrite contain two types of micron sized silicate melt inclusions: clear glass (type I) and devitrified glass (type II) inclusions. Many of the type I inclusions contain a gas bubble of variable size. Type II inclusions can be transparent (IIa), with or without a gas bubble, and brown (type IIb), with a gas bubble. A number of inclusions were measured with the Raman microprobe to detect possible presence of carbon. Carbon in the form of graphite was detected only in type II inclusions. Compositions of 11 inclusions were determined with the electron microprobe and proton microprobe in search for possible explanation of this preference of carbon for devitrified inclusions. All of the measured inclusions are rich in Si, Al and Ca. No significant differences between the compositions of the two types of inclusions were found. The data suggest that the inclusions formed from the melt trapped in growing olivine crystals, which themselves crystallized from a silicon rich, gas bearing melt. There is no coherent relation between the occurrence of graphite and the gas abundance in the original melt, as indicated by the sizes of gas bubbles. Therefore, carbon was not combined in a gaseous species ( e.g. , CO). It must have been preferentially dissolved in some domains of the melt.