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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