Lw. Diamond, SALINITY OF MULTIVOLATILE FLUID INCLUSIONS DETERMINED FROM CLATHRATE HYDRATE STABILITY, Geochimica et cosmochimica acta, 58(1), 1994, pp. 19-41
Measurements of the final dissociation temperature of gas-clathrate hy
drates (Tm(CLA)) are routinely used to determine the salinity of fluid
inclusions which contain a volatile component in addition to water. T
raditionally, experimental data are used to quantitatively relate Tm(C
LA) to the inclusion electrolyte concentration. Because of limitations
in the experimental database, however, this method has hitherto not b
een applicable to the multivolatile fluid inclusions that are common i
n crustal rocks. A general solution to this problem is provided by sta
tistical thermodynamics predictions of multivolatile clathrate stabili
ty. Published theoretical models explicitly account for the effect of
aqueous NaCl in depressing the stability of clathrates composed of any
mixture Of CO2, N2, H2S, CH4, and higher-order hydrocarbons. Analysis
of phase relations in complex clathrate systems shows that such theor
etical predictions yield model salinities if the following fluid inclu
sion data are available: (1) the identity of the phase assemblage at T
m(CLA), (2) the relative concentrations of the volatile species, and (
3) either the homogenization temperature of the volatile fluid fractio
n (bubble point or dew point, either stable or metastable), or an inde
pendent estimate of internal pressure at Tm(CLA). Additional data on f
luid inclusion cation ratios can be incorporated in the calculations t
o recast equivalent weight percent aqueous NaCl in terms of effective
electrolyte concentrations. New experimental data on mixed N2-CO2 clat
hrates, obtained from synthetic fluid inclusions, provide a test of bo
th the model predictions and of the analytical procedure proposed for
natural fluid inclusions. While the accuracy of the predictions varies
between volatile compositions, the uncertainties in the salinities de
rived from the statistical thermodynamics method are generally of the
order acceptable for geochemical applications. Applications to multivo
latile, multi-electrolyte fluid inclusions from gold-quartz deposits i
llustrate the practical operations involved in determining salinity.