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• W2022304725 endingPage "2456" @default.
• W2022304725 startingPage "2451" @default.
• W2022304725 abstract "Halite solubility along part of the vapor-saturated liquidus in the system NaCl-CaCl2-H2O has been determined using the synthetic fluid inclusion technique. Data allow the construction of liquidus isotherms for temperatures up to 500°C and bulk compositions containing >60 wt% total salt and as much as 25 wt% CaCl2. Combined with previous data for the binary system NaCl-H2O and for the ternary system NaCl-CaCl2-H2O in the low-salinity, low-temperature region, a preliminary ternary phase diagram can be constructed that remains incomplete only in the CaCl2-rich region. Results are applied to the interpretation of saline fluid inclusions from quartz veins in oceanic metagabbros, and can be applied to many other natural inclusions containing aqueous solutions with NaCl and CaCl2 the dominant solutes. Microthermometric measurements at equilibrium of the melting temperature of ice [Tm (ice)] and of the dissolution temperature of halite [Tm (halite)] are sufficient to determine the bulk composition of the NaCl-CaCl2-H2O fluid." @default.
• W2022304725 created "2016-06-24" @default.
• W2022304725 creator A5017362466 @default.
• W2022304725 creator A5045784385 @default.
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• W2022304725 date "1988-10-01" @default.
• W2022304725 modified "2023-10-16" @default.
• W2022304725 title "Synthetic fluid inclusions: VIII. Vapor-saturated halite solubility in part of the system NaCl-CaCl2-H2O, with application to fluid inclusions from oceanic hydrothermal systems" @default.
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• W2022304725 doi "https://doi.org/10.1016/0016-7037(88)90303-1" @default.
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