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Douglas Smith Olivine thermometry and source constraints for mantle fragments in the Navajo Volcanic Field, Colorado Plateau, southwest United States: Implications for the mantle wedge Geochemistry, Geophysics, Geosystems 14

Version of Record online: 28 MAR 2013 | DOI: 10.1002/ggge.20065

Key Points

  • Trace-element olivine thermometry works for diverse assemblages in cool mantle
  • The central Colorado Plateau lithosphere to 150 km was mostly cold at 25 m.y
  • Eroded forearc rock was emplaced into that lithosphere by Farallon subduction

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