News and Views


Nature Geoscience 1, 648 - 650 (2008)
doi:10.1038/ngeo327

Subject Category: Volcanology, mineralogy and petrology

Mineral physics: The spin deep within

Stephen Stackhouse1

  1. Stephen Stackhouse is in the Department of Geological Sciences, University of Michigan, 2534 CC Little Bldg, 1100 North University Avenue, Ann Arbor, Michigan 48109-1005, USA.
    e-mail: sstackho@umich.edu


The electronic configuration of iron impurities in lower-mantle minerals influences their physical properties, but it is not well constrained. New studies suggest that ferrous iron in silicate phases exists mainly in an intermediate spin state.

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