Diamonds sampled by plumes from the core-mantle boundary

Trond H Torsvik1, Kevin Burke, Bernhard Steinberger

  • 1Physics of Geological Processes and Geosciences, University of Oslo, Blindern, 0316 Oslo, Norway. trond.torsvik@ngu.no

Nature
|July 16, 2010
PubMed
Summary

Kimberlite eruptions, the primary source of diamonds, are linked to deep mantle structures. Future diamond exploration should focus on ancient cratons overlying these stable, deep-earth zones.

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