Boron, bromine, and other trace elements as clues to the fate of chlorine in mid-ocean ridge vent fluids
- 1 August 1990
- journal article
- Published by Elsevier in Geochimica et Cosmochimica Acta
- Vol. 54 (8) , 2235-2245
- https://doi.org/10.1016/0016-7037(90)90048-p
Abstract
No abstract availableThis publication has 47 references indexed in Scilit:
- The critical point and two-phase boundary of seawater, 200–500°CPublished by Elsevier ,2002
- Halide systematics of submarine hydrothermal ventsNature, 1989
- Supercritical two-phase separation of hydrothermal fluids in the Troodos ophioliteNature, 1988
- Metal-depleted root zones of the Troodos ore-forming hydrothermal systems, CyprusEarth and Planetary Science Letters, 1987
- Two-phase separation and fracturing in mid-ocean ridge gabbros at temperatures greater than 700°CEarth and Planetary Science Letters, 1987
- Geometry, conditions and timing of off-axis hydrothermal metamorphism and ore-deposition in the Solea grabenNature, 1987
- Vertical variations in the effects of hydrothermal metamorphism in Chilean ophiolites: Their implications for ocean floor metamorphismTectonophysics, 1979
- High-Pressure Dissociation of Carbonic and Boric Acids in SeawaterScience, 1967
- The system H 2 O-NaCl at elevated temperatures and pressuresAmerican Journal of Science, 1962
- Electronegativity values from thermochemical dataJournal of Inorganic and Nuclear Chemistry, 1961