The critical point and two-phase boundary of seawater, 200–500°C-Reference-Cited by-同舟云学术

The critical point and two-phase boundary of seawater, 200–500°C

Published:1984-04 Issue:1 Volume:68 Page:172-180
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Bischoff James L.,Rosenbauer Robert J.

Publisher

Elsevier BV

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference15 articles.

1. Geothermal system at 21°N, East Pacific Rise: physical limits on geothermal fluid and role of adiabatic expansion;Bischoff;Science,1980

2. Methane and hydrogen in East Pacific Rise hydrothermal fluids;Welhan;Geophys. Res. Lett.,1979

3. The system H2ONaCl at elevated temperatures and pressures;Sourirajan;Am. J. Sci.,1962

4. Application of the physico-chemical properties of boiling bitterns to the interpretation of brine migration experiments related to salt repositories;Clynne,1980

5. A note on the chemistry of seawater in the range 350°–500°C;Bischoff;Geochim. Cosmochim. Acta,1982

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