Stable isotope signatures of water-rock interaction in mid-ocean ridge hydrothermal systems: Sulfur, oxygen, and hydrogen

Author:

Bowers Teresa Suter

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

Reference45 articles.

1. Geochemistry of hydrothermally altered basalts; Deep Sea Drilling Project hole 504B, leg 83;Alt;Initial Rep. Deep Sea Drill. Proj.,1985

2. Occurrence and origin of anhydrite from Deep Sea Drilling Project leg 70, hole 504B, Costa Rica Rift;Alt;Initial Rep. Deep Sea Drill Proj.,1983

3. Geochemistry of sulfur in a 1.3km section of hydrothermally altered oceanic crust, DSDP hole 504B;Alt;Geochim. Cosmochim. Acta,1989

4. The mineralogy, chemistry, and stable isotopic compositions of hydrothermally altered sheeted dikes: ODP hole 504B, leg 111;Alt,1989

5. On the effect of low-temperature seawater-basalt interaction on the distribution of sulfur in oceanic crust, layer 2;Andrews;Earth Planet. Sci. Lett.,1979

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