Chemistry of submarine hydrothermal solutions at 21 °N, East Pacific Rise
- 1 November 1985
- journal article
- Published by Elsevier BV in Geochimica et Cosmochimica Acta
- Vol. 49 (11), 2197-2220
- https://doi.org/10.1016/0016-7037(85)90222-4
Abstract
No abstract availableThis publication has 46 references indexed in Scilit:
- Sulfur isotope systematics at the 21°N site, East Pacific RiseEarth and Planetary Science Letters, 1983
- Distribution of elements in sea waterEos, 1983
- East Pacific Rise Near 13°N: Geology of New Hydrothermal FieldsScience, 1983
- On the fate of sulfate during hydrothermal circulation at mid-ocean ridgesEarth and Planetary Science Letters, 1982
- East Pacific rise at 21°N: The volcanic, tectonic, and hydrothermal processes of the central axisEarth and Planetary Science Letters, 1981
- Hot spring deposits on the East Pacific Rise at 21°N: preliminary description of mineralogy and genesisEarth and Planetary Science Letters, 1981
- The mineralogy and the isotopic composition of sulfur in hydrothermal sulfide/sulfate deposits on the East Pacific Rise, 21°N latitudeEarth and Planetary Science Letters, 1981
- A high-temperature hydrothermal deposit on the seabed at a gulf of California spreading centerEarth and Planetary Science Letters, 1980
- Hydrothermal heat flux of the “black smoker” vents on the East Pacific RiseEarth and Planetary Science Letters, 1980
- K, Rb, Cs contents and K/Rb, K/Cs ratios of fresh and altered submarine basaltsEarth and Planetary Science Letters, 1969