Modeling of hydrogen production by serpentinization in ultramafic-hosted hydrothermal systems: application to the Rainbow field
Author:
Affiliation:
1. Laboratoire des Sciences du Climat et de l'Environnement; UMR 8212 CEA-CNRS-UVSQ; Gif-sur-Yvette Cedex France
2. Département Géosciences Marines; IFREMER Brest; Plouzané France
Publisher
Wiley
Subject
General Earth and Planetary Sciences
Link
http://onlinelibrary.wiley.com/wol1/doi/10.1111/gfl.12169/fullpdf
Reference67 articles.
1. Agrinier P Cannat M 1997 Oxygen-isotope constraints on serpentinization processes in ultramafic rocks from the Mid-Atlantic Ridge (23°N) 596 College Station, TX, United States
2. Compositional controls on vent fluids from ultramafic-hosted hydrothermal systems at mid-ocean ridges: an experimental study at 400°C, 500 bars;Allen;Geochimica et Cosmochimica Acta,2003
3. Serpentinization and heat generation: constraints from Lost City and Rainbow hydrothermal systems;Allen;Geochimica et Cosmochimica Acta,2004
4. A microstructural study of a « crack-seal » type serpentine vein using SEM and TEM techniques;Andreani;European Journal of Mineralogy,2004
5. Hydrothermal cooling of midocean ridge axes: do measured and modeled heat fluxes agree?;Baker;Earth and Planetary Science Letters,2007
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