Hydrogen isotope systematics of phase separation in submarine hydrothermal systems: Experimental calibration and theoretical models
Hydrogen isotope fractionation factors were measured for coexisting brines and vapors formed by phase separation of NaCl/H 2O fluids at temperatures ranging from 399–450°C and pressures from 277–397 bars. It was found that brines are depleted in D compared to coexisting vapors at all conditions stud...
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Veröffentlicht in: | Geochimica et cosmochimica acta 1996-05, Vol.60 (9), p.1595-1604 |
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