| Item type |
学術雑誌論文 / Journal Article(1) |
| 公開日 |
2007-06-19 |
| タイトル |
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|
タイトル |
A preliminary study of ice core chronology at Dome Fuji Station, Antarctica |
|
言語 |
en |
| 言語 |
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言語 |
eng |
| 資源タイプ |
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資源 |
http://purl.org/coar/resource_type/c_6501 |
|
タイプ |
journal article |
| アクセス権 |
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アクセス権 |
open access |
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アクセス権URI |
http://purl.org/coar/access_right/c_abf2 |
| 著者 |
Watanabe, Okitsugu
Fujii, Yoshiyuki
Motoyama, Hideaki
Furukawa, Teruo
Shoji, Hitoshi
Enomoto, Hiroyuki
Kameda, Takao
Narita, Hideki
Naruse, Renji
Hondoh, Takeo
Fujita, Shuji
Mae, Shinji
Azuma, Nobuhiko
Kobayashi, Shun'ichi
Nakawo, Masayoshi
Ageta, Yutaka
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| 著者別名 |
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識別子Scheme |
WEKO |
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識別子 |
36778 |
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姓名 |
庄子, 仁 |
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言語 |
ja |
| 著者別名 |
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識別子Scheme |
WEKO |
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識別子 |
36779 |
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姓名 |
榎本, 浩之 |
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言語 |
ja |
| 著者別名 |
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識別子Scheme |
WEKO |
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識別子 |
44128 |
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|
識別子Scheme |
NRID |
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識別子URI |
https://nrid.nii.ac.jp/nrid/1000000233974 |
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識別子 |
1000000233974 |
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姓名 |
亀田, 貴雄 |
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言語 |
ja |
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姓名 |
Kameda, Takao |
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言語 |
en |
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姓 |
亀田 |
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言語 |
ja |
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姓 |
Kameda |
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言語 |
en |
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名 |
貴雄 |
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言語 |
ja |
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名 |
Takao |
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言語 |
en |
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識別子Scheme |
ISNI |
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識別子URI |
https://www.isni.org/isni/ |
| 抄録 |
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内容記述タイプ |
Abstract |
|
内容記述 |
A 112．59 m-deep ice core was drilled at Dome Fuji Station by a JARE-34 party in 1993 when a pilot hole was prepared for a deep core drilling operation．A preliminary examination was made for ice core chronology by two signals： one electric conductivity peaks measured in the home laboratory and the other field observation results obtained by JARE-36 party on the deeper part of the core. The electric conductivity peak analyses suggest the same 5 volcanic eruptions, in 1464 AD, 1259 AD, 865 AD, 639 AD and 346 BC, reported for the ice core of Byrd Camp, Antarctica．Field observations for ECM and crystal size distributions suggest that the period 374 m depth level corresponds to the end of Wisconsin ice period The results suggest that accumulation rate at Dome Fuji Station is between 2.5 and 3.O cm of water equivalent/year, and the end of Wisconsin-Holocene Transition will be found between depths of 340 and 400 m．The depth-age curves for the core at Dome Fuji Station are obtained from the surface （at present） to 400 m （at 12000 years BP）. |
| 書誌情報 |
Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology
巻 11,
p. 9-13
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| 権利 |
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権利情報 |
NATIONAL INSTITUTE OF POLAR RESEARCH, Watanabe, O., Y. Fujii, H. Motoyama, T. Furukawa, H. Shoji, H. Enomoto, T. Kameda, H. Narita, R. Naruse,T. Hondoh, S. Fujita, S. Mae, N. Azuma, S. Kobayashi, M. Nakawo and Y. Ageta, Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology, 11, 1997, 9-13 |
| フォーマット |
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内容記述タイプ |
Other |
|
内容記述 |
application/pdf |
| 出版者 |
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出版者 |
国立極地研究所 |
|
言語 |
ja |
| 著者版フラグ |
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|
言語 |
en |
|
値 |
publisher |
| 出版タイプ |
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出版タイプ |
VoR |
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出版タイプResource |
http://purl.org/coar/version/c_970fb48d4fbd8a85 |
5126.pdf (1.6 MB)
