Iron Partitioning and Density Changes of Pyrolite in Earth’s Lower Mantle

@article{Irifune2010IronPA,
  title={Iron Partitioning and Density Changes of Pyrolite in Earth’s Lower Mantle},
  author={T. Irifune and T. Shinmei and C. McCammon and N. Miyajima and D. Rubie and D. Frost},
  journal={Science},
  year={2010},
  volume={327},
  pages={193 - 195}
}
Spin Transitions and Mantle Phases The extreme temperatures and pressures at depth can cause mantle minerals to undergo phase transformations. For example, it is thought that an electronic spin transition that occurs at high pressures in the lower mantle leads to the partitioning of various iron mineral phases. Using a multianvil apparatus to study a synthetic material similar in composition to the lower mantle, Irifune et al. (p. 193, see the Perspective by Hirose; published online 3 December… Expand
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