SYNTHETIC FLUID INCLUSIONS IN THE SYSTEMS NACL-H2O AND NACL-CO2-H2O: DISSOLUTION TEMPERATURES OF HALITE

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dc.contributor.author Nagaseki H.
dc.contributor.author Hayashi K.-I.
dc.date.accessioned 2025-04-05T07:16:10Z
dc.date.available 2025-04-05T07:16:10Z
dc.date.issued 2006
dc.identifier https://elibrary.ru/item.asp?id=14122396
dc.identifier.citation Resource Geology, 2006, 56, 2, 133-140
dc.identifier.issn 1344-1698
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/48806
dc.description.abstract This study examined the effect Of CO2 on NaCl solubility in hydrothermal fluid, with the synthetic fluid inclusion technique. Fluid inclusions of 30-40 wt% NaCl and 5 mol % CO2 were synthesized, and their halite dissolution temperatures, Tm,(halite), were measured. The solubilities of NaCl in CO2-bearing aqueous fluid were obtained at 160-320°C under vapor-saturated pressures. The Tm(halite) value in aqueous fluid with 5 mol % CO2 obtained in this study agrees with that of Schmidt et al. (1995), showing that 5 mol % CO2 reduces the solubility of NaCl by about 1 wt%. Calculation of magnetite solubility suggests that 5-10 mol % CO2 decreases magnetite solubility by 4.5-8.9 % relative to the magnetite solubility in CO2-free solution. Therefore, an increase of CO2 content in ore-forming solutions may cause deposition of iron minerals and produce ore deposits.
dc.subject EFFECT OF CO2
dc.subject HALITE SOLUBILITY
dc.subject NACL-CO2-H2O SYSTEM
dc.subject SYNTHETIC FLUID INCLUSION
dc.title SYNTHETIC FLUID INCLUSIONS IN THE SYSTEMS NACL-H2O AND NACL-CO2-H2O: DISSOLUTION TEMPERATURES OF HALITE
dc.type Статья
dc.identifier.doi 10.1111/j.1751-3928.2006.tb00274.x


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