The determination of phase relations in the CH4 H2O NaCl system at 1 kbar, 400 to 600° C using synthetic fluid inclusions

WM Lamb, RK Popp, LA Boockoff - Geochimica et Cosmochimica Acta, 1996 - Elsevier
Synthesis of fluid inclusions in the CH4 H2O NaCl system was accomplished by
subjecting fractured quartz, along with known quantities of CH4, H2O, and NaCl, to a …

Phase relations in the CH4-H2O-NaCl system at 2 kbar, 300 to 600 C as determined using synthetic fluid inclusions

WM Lamb, CJ Mcshane, RK Popp - Geochimica et Cosmochimica Acta, 2002 - Elsevier
Synthesis of fluid inclusions in the CH4-H2O-NaCl system was accomplished by subjecting
fractured quartz or fluorite, along with known quantities of CH4, H2O, and NaCl, to a …

Synthetic fluid inclusions in natural quartz. III. Determination of phase equilibrium properties in the system H2O-NaCl to 1000 C and 1500 bars

RJ Bodnar, CW Burnham, SM Sterner - Geochimica et Cosmochimica Acta, 1985 - Elsevier
Phase equilibria in the system H 2 O-NaCl have been determined to 1000° C and 1500 bars
using synthetic fluid inclusions formed by healing fractures in inclusion-free Brazilian quartz …

The compositional limits of fluid immiscibility in the system H2O NaCl CO2 as determined with the use of synthetic fluid inclusions in conjunction with mass …

JD Frantz, RK Popp, TC Hoering - Chemical Geology, 1992 - Elsevier
The compositional limits of fluid immiscibility in the system NaCl H 2 O CO 2 were
investigated from 500° to 700° C at pressures of 1, 2 and 3 kbar. Synthetic fluid inclusions …

Synthetic fluid inclusions: XII. The system H2O NaCl. Experimental determination of the halite liquidus and isochores for a 40 wt% NaCl solution

RJ Bodnar - Geochimica et Cosmochimica Acta, 1994 - Elsevier
The slopes of the liquidus and lines of constant liquid-vapor homogenization temperature
(iso-Th) in PT space for a 40 wt% NaCl bulk composition in the H 2 O-NaCl system were …

Synthetic fluid inclusions: XIII. Experimental determination of PVT properties in the system H2O+ 40 wt% NaCl+ 5 mol% C02 at elevated temperature and pressure

C Schmidt, KM Rosso, RJ Bodnar - Geochimica et Cosmochimica Acta, 1995 - Elsevier
The location of the liquid+ vapor→ liquid phase boundary and the P− T slopes of iso-Th
lines were determined for a constant composition of 40±0.1 wt% NaCl and 5±0.15 mol …

Synthetic fluid inclusions XVIII: Experimental determination of the PVTX properties of H2O–CH4 to 500° C, 3 kbar and XCH4⩽ 4 mol.%

F Lin, RJ Bodnar - Geochimica et Cosmochimica Acta, 2010 - Elsevier
The pressure–volume–temperature–composition (PVTX) properties of H2O–CH4 were
determined from the bubble point curve to 500° C and 3 kbar for compositions⩽ 4mol …

Determination of the homogenization temperatures and densities of supercritical fluids in the system NaClKClCaCl2H2O using synthetic fluid inclusions

YG Zhang, JD Frantz - Chemical Geology, 1987 - Elsevier
Synthetic fluid inclusions were experimentally produced by equilibrating small fractured
prisms of quartz with aqueous solutions at temperatures from 300° to 700° C and pressures …

Synthetic fluid inclusions. V. Solubility relations in the system NaCl-KCl-H2O under vapor-saturated conditions

SM Sterner, DL Hall, RJ Bodnar - Geochimica et Cosmochimica Acta, 1988 - Elsevier
Vapor-saturated solubility relationships in the system NaCl-KCl-H 2 O have been
determined by experimentally synthesizing fluid inclusions in quartz in the presence of …

Synthetic fluid inclusions: XVI. PVTX properties in the system H2O-NaCl-CO2 at elevated temperatures, pressures, and salinities

C Schmidt, RJ Bodnar - Geochimica et Cosmochimica Acta, 2000 - Elsevier
The ternary system H2O-NaCl-CO2 is one of the most important fluid systems in
geochemistry and petrology. However, there is little information on the phase equilibrium …