A 6-year time series of hydrothermal plumes over the Cleft segment of the Juan de Fuca Ridge

Author:

Baker Edward T.

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Earth-Surface Processes,Geochemistry and Petrology,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry,Oceanography,Geophysics

Reference51 articles.

1. The distribution of hydrothermal venting along the East Pacific Rise, 8°45′ to 11°50′N, and its relationship to geophysical characteristics of the ridge;Baker;Eos Trans. AGU,1992

2. Hydrothermal venting and the apparent magmatic budget of the Juan de Fuca Ridge;Baker;J. Geophys. Res.,1992

3. Changes in submarine hydrothermal 3He/heat ratios as an indicator of magmatic/tectonic activity;Baker;Nature,1990

4. Hydrothermal plume measurements: A regional perspective;Baker;Science,1986

5. Characteristics of hydrothermal plumes from two vent fields on the Juan de Fuca Ridge, northeast Pacific Ocean;Baker;Earth Planet. Sci. Lett.,1987

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