@article{oai:nipr.repo.nii.ac.jp:00002892,
 author = {ワタナベ, オキツグ and フジイ, ヨシユキ and カミヤマ, コキチ and モトヤマ, ヒデアキ and フルカワ, テルオ and イガラシ, マコト and コウノ, ミカ and カナモリ, サトル and カナモリ, ノブコ and アゲタ, ユタカ and ナカオ, マサヨシ and タナカ, ヒロシ and サトウ, カズヒデ and ショウジ, ヒトシ and カワムラ, キミタカ and マトバ, スミト and シマダ, ワタル and WATANABE, Okitsugu and FUJII, Yoshiyuki and KAMIYAMA, Kokichi and MOTOYAMA, Hideaki and FURUKAWA, Teruo and IGARASHI, Makoto and KOHNO, Mika and KANAMORI, Satoru and KANAMORI, Nobuko and AGETA, Yutaka and NAKAWO, Masayoshi and TANAKA, Hiroshi and SATOW, Kazuhide and SHOJI, Hitoshi and KAWAMURA, Kimitaka and MATOBA, Sumito and SHIMADA, Wataru},
 journal = {Polar meteorology and glaciology},
 month = {Dec},
 note = {P(論文), 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.},
 pages = {83--89},
 title = {BASIC ANALYSES OF DOME FUJI DEEP ICE CORE PART 1 : STABLE OXYGEN AND HYDROGEN ISOTOPE RATIOS, MAJOR CHEMICAL COMPOSITIONS AND DUST CONCENTRATION},
 volume = {13},
 year = {1999}
}