A note on the chemistry of seawater in the range 350°–500°C
Author:
Publisher
Elsevier BV
Subject
Geochemistry and Petrology
Reference12 articles.
1. Geothermal system at 21°N, East Pacific Rise: Physical limits on geothermal fluid and role of adiabatic expansion;Bischoff;Science,1980
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3. Geothermai system at 21°N;Chen;Science,1981
4. An oxygen isotope profile in a section of Cretaceous oceanic crust, Samail ophiolite, Oman: evidence for δ18 oxygen buffering of the oceans by deep (> 5 km) seawater-hydrothermal circulation at mid-ocean ridges;Gregory;J. Geophys. Res.,1981
5. Hot spring deposits on the East Pacific Rise at 21 °N: Preliminary description of mineralogy and genesis;Haymon;Earth Planet. Sci. Lett.,1981
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