Sulfur isotope evidence for microbial sulfate reduction in altered oceanic basalts at ODP Site 801-Reference-Cited by-同舟云学术

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Sulfur isotope evidence for microbial sulfate reduction in altered oceanic basalts at ODP Site 801

Published:2008-04 Issue:1-2 Volume:268 Page:110-123
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Rouxel Olivier,Ono Shuhei,Alt Jeff,Rumble Douglas,Ludden John

Publisher

Elsevier BV

Subject

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

Reference64 articles.

1. Sulfur isotopic profile through the oceanic crust: sulfur mobility and seawater–crustal sulfur exchange during hydrothermal alteration;Alt;Geology,1995

2. Sulfur in pacific deep-sea sediments (Leg 129) and implications for cycling of sediment in subduction zones;Alt,1992

3. Sulfur in serpentinized oceanic peridotites: serpentinization processes and microbial sulfate reduction;Alt;J. Geophys. Res.,1998

4. The uptake of carbon during alteration of ocean crust;Alt;Geochim. Cosmochim. Acta,1999

5. Hydrothermal alteration of upper oceanic crust formed at a fast-spreading ridge: mineral, chemical, and isotopic evidence from ODP Site 801;Alt;Chem. Geol.,2003

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