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C. Geoffrey Wheat, Samuel M. Hulme, Andrew T. Fisher, Beth N. Orcutt and Keir Becker Seawater recharge into oceanic crust: IODP Exp 327 Site U1363 Grizzly Bare outcrop Geochemistry, Geophysics, Geosystems 14

Version of Record online: 17 JUN 2013 | DOI: 10.1002/ggge.20131

Key Points

  • Warm, highly altered fluids lie 50 meters from Grizzly Bare outcrop
  • Fluid flow within upper basaltic crust is complex and compartmentalized
  • Redox gradients near zones of seawater inflow affect microbial populations

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