The history of serpentinisation at mid-ocean ridges: Insights from in situ trace elements coupled with oxygen and boron isotopes

Author:

Vesin Coralie,Rubatto Daniela,Pettke Thomas

Funder

Swiss National Science Foundation

Publisher

Elsevier BV

Reference76 articles.

1. Oxygen-isotope constraints on serpentinization processes in ultramafic rocks from the Mid-Atlantic Ridge (23°N);Agrinier;Notes,1997

2. Hydrothermal alteration of the peridotites cored at the ocean/continent boundary of the Iberian margin: petrologic and stable isotope evidence;Agrinier;Proc. Ocean Drill. Program Sci. Results,1988

3. O and H stable isotope compositions of oceanic crust and upper mantle rocks exposed in the Hess deep near the Galapagos Triple Junction;Agrinier;Earth Planet. Sci. Lett.,1995

4. Mineralogical and oxygen isotopic features of serpentinites recovered from the ocean/continent transition in the Iberia Abyssal Plain;Agrinier;Proc. Ocean Drill. Program, 149 Sci Res.,1996

5. Compositional controls on vent fluids from ultramafic-hosted hydrothermal systems at mid-ocean ridges: an experimental study at 4 00°C, 500 bars;Allen;Geochim. Cosmochim. Acta,2003

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