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Ingo Grevemeyer, Timothy J. Reston and Stefan Moeller Microseismicity of the Mid-Atlantic Ridge at 7°S–8°15′S and at the Logatchev Massif oceanic core complex at 14°40′N–14°50′N Geochemistry, Geophysics, Geosystems 14

Version of Record online: 5 SEP 2013 | DOI: 10.1002/ggge.20197

Key Points

  • Seismicity yielded that earthquakes generally occur at the axis axis
  • At Logatchev Massif seismicity is shifted away from the ridge axis
  • Location of the Logatchev vents is controlled by faulting and serpentinization

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