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- W1528070337 abstract "Microanalytical techniques such as SEM, EDX, and EMA have been shown to be ideal in determining the host phases of the minor and trace elements in the Chattanooga shale. Positive correlations were found between pyrite and organic constituents. However, these observations provided no evidence that micro-organisms acted as hosts for pyrite framboids. It is interesting that appreciable organic sulfur is still present, which suggests that the sulfur used for the formation of pyrite must have been derived mostly from other sources. It may be that the sulfate-reducing bacteria had an affinity for organic matter and that the organic fragments acted as substrates for pyrite growth." @default.
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- W1528070337 date "1982-01-01" @default.
- W1528070337 modified "2023-09-27" @default.
- W1528070337 title "Application of scanning electron microscopy and ultraviolet fluorescence to a study of Chattanooga shale specimens" @default.
- W1528070337 hasPublicationYear "1982" @default.
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