An assessment of the accuracy of isochore location techniques for H2O-CO2-NaCl fluids at granulite facies pressure-temperature conditions☆
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Cited by (12)
A predictive model for the PVTx properties of CO<inf>2</inf>-H<inf>2</inf>O-NaCl fluid mixture up to high temperature and high pressure
2015, Applied GeochemistryCitation Excerpt :In particular, the isochores of CO2–H2O–NaCl fluid inclusions, along which the fluid inclusions were trapped, are often calculated from the pressure–volume–temperature–composition (PVTx) models (Bakker, 1999; Brown and Lamb, 1989; Duan et al., 2008; Mao et al., 2010; Sun and Dubessy, 2012). In the near decades, there have been some experimental studies for the PVTx properties of CO2–H2O–NaCl fluid mixture (Gehrig et al., 1986; Johnson, 1992; Li et al., 2004; Nighswander et al., 1989; Schmidt and Bodnar, 2000; Schmidt et al., 1995; Song et al., 2005, 2013; Teng and Yamasaki, 1998; Yan et al., 2011). However, these data are very scattered, and most of them cover a limited temperature–pressure–composition space that is only valid for CO2 sequestration environments, and they are inconvenient and inadequate for fluid inclusion research.
Synthetic fluid inclusions: XVI. PVTX properties in the system H<inf>2</inf>O-NaCl-CO<inf>2</inf> at elevated temperatures, pressures, and salinites
2000, Geochimica et Cosmochimica Acta
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Presented at PACROFI III, Third Biennial Pan-American Conference on Research on Fluid Inclusions, held in Toronto, Canada, May 20–22, 1990.