Site of Preference Energy and Selective Uptake of Transition-Metal Ions from a Magma

DOI Web Site 被引用文献3件
  • Roger G. Burns
    Department of Geology and Geophysics, University of California, Berkeley
  • William S. Fyfe
    Department of Geology and Geophysics, University of California, Berkeley

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<jats:p>Results of absorption spectra measurements on silicate glasses of various compositions indicate that ions of the first transition-metal series are present in tetrahedral and octahedral sites in silicate melts (glasses). The fractionation patterns observed for transition-metal ions between magmas and silicate minerals can be interpreted according to crystal field theory in terms of octahedral "site preference energies" of transition ions in crystal lattices.</jats:p>

収録刊行物

  • Science

    Science 144 (3621), 1001-1003, 1964-05-22

    American Association for the Advancement of Science (AAAS)

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