Basic analyses of Dome Fuji deep ice core Part 1 : Stable oxygen and hydrogen isotope ratios, major chemical compositions and dust concentration

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Basic chemical analyses of a 2503m deep ice core obtained at Dome Fuji Station, Antarctica in 1995-1996 were carried out to determine stable oxygen and hydrogen isotope ratios, major chemical compositions and microparticle concentrations. We here describe the analytical procedure and the results as well as the determination of working time scale. The ice core covers the past 340ka which includes three glacial-interglacial cycles clearly shown by the stable oxygen isotope profile. Major chemical compositions and microparticle concentrations larger than 0.52μm show high concentrations in glacials and low in interglacials.

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詳細情報

  • CRID
    1573668926655185920
  • NII論文ID
    110001135941
  • NII書誌ID
    AA1129795X
  • ISSN
    13443437
  • 本文言語コード
    en
  • データソース種別
    • CiNii Articles
    • Crossref

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