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C. Mallows and R. C. Searle A geophysical study of oceanic core complexes and surrounding terrain, Mid-Atlantic Ridge 13°N–14°N Geochemistry, Geophysics, Geosystems 13

Version of Record online: 6 JUN 2012 | DOI: 10.1029/2012GC004075

Key Points

  • Core complexes occur with low regional melt supply and high tectonic strain
  • Core complex footwalls are capped by low density zones of gabbro or serpentinite
  • Poorly lineated magnetic anomalies imply heterogeneous lithology or spreading

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