Stable isotope (δ18O, δD, δ37Cl) evidence for multiple fluid histories in mid-Atlantic abyssal peridotites (ODP Leg 209)
Author:
Publisher
Elsevier BV
Subject
Geochemistry and Petrology,Geology
Reference54 articles.
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2. Stable isotope compositions of serpentinite seamounts in the Mariana forearc: serpentinization processes, fluid sources and sulfur metasomatism;Alt;Earth and Planetary Science Letters,2006
3. Hydrothermal alteration and microbial sulfate reduction in peridotite and gabbro exposed by detachment faulting at the Mid-Atlantic Ridge, 15°20N (ODP Leg 209): a sulfur and oxygen isotope study;Alt;Geochemistry Geophysics Geosystems,2007
4. Silica metasomatism of oceanic serpentinites;Bach,2007
5. Seawater-peridotite interactions: first insights from ODP Leg 209, MAR 15°N;Bach;Geochemistry Geophysics Geosystems,2004
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