Geochemistry of hydrothermal fluids from Axial Seamount hydrothermal emissions study vent field, Juan de Fuca Ridge: Subseafloor boiling and subsequent fluid‐rock interaction
- 10 August 1990
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 95 (B8), 12895-12921
- https://doi.org/10.1029/jb095ib08p12895
Abstract
No abstract availableKeywords
This publication has 46 references indexed in Scilit:
- Infrared spectroscopic measurements of CO2 and H2O in Juan de Fuca Ridge basaltic glassesEarth and Planetary Science Letters, 1988
- Supercritical two-phase separation of hydrothermal fluids in the Troodos ophioliteNature, 1988
- Phase separation in seafloor geothermal systems; an experimental study of the effects on metal transportAmerican Journal of Science, 1987
- Boron isotope exchange between seawater and the oceanic crustGeochimica et Cosmochimica Acta, 1987
- Two-phase separation and fracturing in mid-ocean ridge gabbros at temperatures greater than 700°CEarth and Planetary Science Letters, 1987
- An empirical equation of state for hydrothermal seawater (3.2 percent NaCl)American Journal of Science, 1985
- Hydrothermal vents on an axis seamount of the Juan de Fuca ridgeNature, 1985
- The critical point and two-phase boundary of seawater, 200–500°CEarth and Planetary Science Letters, 1984
- Methane and hydrogen in East Pacific Rise hydrothermal fluidsGeophysical Research Letters, 1979
- The system H 2 O-NaCl at elevated temperatures and pressuresAmerican Journal of Science, 1962