Phase Equilibria in Subseafloor Hydrothermal Systems: a Review of the Role of Redox, Temperature, Ph and Dissolved Cl on the Chemistry of Hot Spring Fluids at Mid-Ocean Ridges-Reference-Cited by-同舟云学术

Phase Equilibria in Subseafloor Hydrothermal Systems: a Review of the Role of Redox, Temperature, Ph and Dissolved Cl on the Chemistry of Hot Spring Fluids at Mid-Ocean Ridges

Published:2013-03-22 Issue: Volume: Page:248-272
ISSN:2328-8779
Container-title:Seafloor Hydrothermal Systems: Physical, Chemical, Biological, and Geological Interactions
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Author:

Seyfried W. E.,Ding Kang

Publisher

American Geophysical Union

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1029/GM091p0248/fullpdf

Reference94 articles.

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2. Boron, bromine, and other trace clements as clues to the fate of chlorine in mid-ocean ridge vent fluids;Berndt;Geochim. Cosmochim. Acta,1990a

3. Quartz dissolution and precipitation rates in neutral to acidic NaCl fluids from 200 to 400°C,400 bars: Application to mid-ocean ridge hydrothermal systems;Berndt;Eos Trans. AGU,1990b

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