Flow rates in the axial hot springs of the East Pacific Rise (21°N): Implications for the heat budget and the formation of massive sulfide deposits

Author:

Converse D.R.,Holland H.D.,Edmond J.M.

Publisher

Elsevier BV

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference67 articles.

1. Forced plumes;Morton;J. Fluid Mech.,1959

2. Helium-3 and manganese at the 21°N East Pacific Rise hydrothermal site;Lupton;Earth Planet. Sci. Lett.,1980

3. Cu-pyrite mineralization and seawater convection in oceanic crust—the ophiolitic ore deposits of Cyprus;Spooner,1980

4. The heat flow through oceanic and continental crust and the heat loss of the Earth;Sclater;Rev. Geophys. Space Phys.,1980

5. Heat flow measured over the Juan de Fuca Ridge: evidence for widespread hydrothermal circulation in a highly heat transportive crust;Davis;J. Geophys. Res.,1977

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