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Anika Husen, Renat R. Almeev, François Holtz, Jürgen Koepke, Takashi Sano and Kurt Mengel Geothermobarometry of basaltic glasses from the Tamu Massif, Shatsky Rise oceanic plateau Geochemistry, Geophysics, Geosystems 14

Version of Record online: 1 OCT 2013 | DOI: 10.1002/ggge.20231

Key Points

  • Tamu Massif (Shatsky Rise) basalts resembling OJP lavas and close to MORBs
  • Differentiation beneath Tamu Massif occured at low pressures (<200 MPa)
  • Shatsky Rise rocks reflect magma storage at different crustal levels

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