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S. C. Wilson, B. J. Murton and R. N. Taylor Mantle composition controls the development of an Oceanic Core Complex Geochemistry, Geophysics, Geosystems 14

Version of Record online: 24 APR 2013 | DOI: 10.1002/ggge.20046

Key points

  • Amagmatic parts of the ridge are currently producing normal amounts of melt
  • Mantle geochemistry triggers a change from magmatism to amagmatism
  • Unusually, the mid-segment lithosphere is cold and thick

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