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Fayalitic olivine composition in an H-type chondrite

  • Soils, Mineralogy, Geology And Archaeology
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Abstract

Low temperature Mössbauer spectroscopy is used to investigate the composition and the iron distribution in the M1 and M2 crystallographic sites of a fayalitic olivine in an H-type chondrite.

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Authors and Affiliations

  1. Instituto de Física, UFRGS, 91540-000, Porto Alegre, RS, Brazil

    M. I. da Costa Jr. & J. I. Kunrath

  2. Departamento de Física, UFCE, 60540-000, Fortaleza, CE, Brazil

    J. C. P. de Oliveira

  3. Instituto de Geociências, UFRGS, 91540-000, Porto Alegre, RS, Brazil

    N. Vieira Jr., J. O. Chies, A. Roisenberg & E. Fernandes de Lima

  4. Departamento de Física, FUEM, 87020-000, Maringá, PR, Brazil

    A. Paesano Jr. & M. L. dos Santos

Authors
  1. M. I. da Costa Jr.
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  2. J. I. Kunrath
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  3. J. C. P. de Oliveira
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  4. N. Vieira Jr.
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  5. J. O. Chies
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  6. A. Roisenberg
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  7. E. Fernandes de Lima
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  8. A. Paesano Jr.
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  9. M. L. dos Santos
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da Costa, M.I., Kunrath, J.I., de Oliveira, J.C.P. et al. Fayalitic olivine composition in an H-type chondrite. Hyperfine Interact 83, 457–461 (1994). https://doi.org/10.1007/BF02074317

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  • DOI: https://doi.org/10.1007/BF02074317

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