Evolution of hydrothermal activity on the Juan de Fuca Ridge: Observations, mineral ages, and Ra isotope ratios

Author:

Stakes Debra,Moore Willard S.

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

Reference44 articles.

1. Influence of magma chamber geometry on hydrothermal activity at mid-ocean ridges;Brikowski;Earth Planet. Sci. Lett.,1989

2. The U-Th-Pb systematics in hot springs on the East Pacific Rise at 21°N and Guaymas Basin;Chen;Geochim. Cosmochim. Acta,1986

3. The origin of metal-bearing submarine hydrothermal solutions;Corliss;J. Geophys. Res.,1971

4. Deer , W. A. R. A. Howie J. Zussman Rock-Forming Minerals 14 Framework Silicates Longmans, Green, Toronto, Ont. 1963

5. Standing pools of 350°C fluid and large seafloor sulfide structures;Delaney;Eos Trans. AGU,1988

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