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- W2266215989 abstract "Liquid-vapour-solid phase inclusions in spodumene (LiAIS20 6) have been interpreted to be the products of a hydrous silicate melt that was entrapped during crystallization. However, recent laser Raman spectroscopic analyses indicate that lithium carbonate is a major component of the entrapped fluid, as shown by the presence of the mineral zabuyelite (Li2C03) in the inclusions. The high carbonate content of these inclusions is inconsistent with previous estimates of fluid composition and is typical of fluid inclusions trapped during a lower temperature hydrothermal stage in granitic rocks. In this study, the bulk composition and origin of fluid inclusions in spodumene from the Tranco pegmatite, Manitoba, were reevaluated on the basis of (I) new petrographic data, (2) laser Raman spectroscopic analyses of solid phases in 300 separate fluid inclusions, and (3) thermodynamic analysis of the stability of the inclusion constituents in the system Li20-" @default.
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- W2266215989 date "1999-01-01" @default.
- W2266215989 modified "2023-09-27" @default.
- W2266215989 title "Abstract: The origin and significance of zabuyelite (Li2CO3)-bearing fluid inclusions in spodumene from granitic pegmatites" @default.
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