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    Intermediate-spin ferrous iron in lowermost mantle post-perovskite and perovskite

    The Earth’s lowermost mantle displays an important mineralogical transition from perovskite to post-perovskite but the spin state of iron in these phases remains poorly known. Experimental results suggest that...

    Jung-Fu Lin, Heather Watson, György Vankó, Esen E. Alp in Nature Geoscience (2008)