Microbial sulfate reduction and the sulfur budget for a complete section of altered oceanic basalts, IODP Hole 1256D (eastern Pacific)

Author:

Alt Jeffrey C.,Shanks Wayne C.

Publisher

Elsevier BV

Subject

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

Reference57 articles.

1. Sulfur geochemistry and microbial sulfate reduction during low-temperature alteration of uplifted lower oceanic crust: insights from ODP Hole 735B;Alford;Chem. Geol.,2011

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

3. Alteration of the upper oceanic crust: mineralogy, chemistry, and processes;Alt,2004

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

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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