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- W1998302541 abstract "Means of extracting and quantitatively analyzing volatiles in fluid inclusions have been studied and details of the methods developed are presented. Thermal decrepitation is the preferred method to open inclusions because experiments indicate that this method yields more accurate measurements of the sulphur-species gases and water. Two assemblages of inclusion species have repeatedly been detected in inclusions from mineral deposits. A CO2-dominated assemblage typically has been measured in inclusions from porphyry-type deposits. A CO2N2CnHn assemblage is typical of inclusion volatiles from sediment-hosted and epithermal deposits. The probable source of N2 and organic compounds is biologic material which is consistent with a crustal source for the ore solutions. Inclusion volatiles from most ore deposits have 1–3 mole% gaseous species. However, levels of 5–15% have been measured in assemblages of vapor-dominant and liquid dominant inclusions from epithermal deposits. The interpretation is that vapor-dominant inclusions are rich in gaseous species. This implies that the indicated “boiling” of the ore solutions was not strictly aqueous boiling but more an unmixing of the gaseous components. Analytical data on volatiles in fluid inclusions have been used to calculate fO2, fS2, fCO2 and pH of ore fluids, and these values agree with values calculated from other data. Data on gases in fluid inclusions have also been used to estimate trapping pressure and study paragenesis." @default.
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- W1998302541 date "1987-03-01" @default.
- W1998302541 modified "2023-10-18" @default.
- W1998302541 title "Analysis of volatiles in fluid inclusions by mass spectrometry" @default.
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- W1998302541 doi "https://doi.org/10.1016/0009-2541(87)90020-9" @default.
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