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Brian E. Tucholke, Susan E. Humphris and Henry J. B. Dick Cemented mounds and hydrothermal sediments on the detachment surface at Kane Megamullion: A new manifestation of hydrothermal venting Geochemistry, Geophysics, Geosystems 14

Version of Record online: 3 SEP 2013 | DOI: 10.1002/ggge.20186

Key Points

  • Hydrothermal circulation occurs in all parts of oceanic detachment-fault systems
  • Low-T venting in detachment footwalls may occur several m.y. off-axis
  • Low-T hydrothermal Fe-Mn minerals appear in rock-debris mounds and layered chalk

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