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  1. F300 宇宙地球環境研究所
  2. F300b 紀要
  3. 名古屋大学加速器質量分析計業績報告書
  4. 25

北海道厚真川下流域の後期更新世~完新世の古環境変遷

https://doi.org/10.18999/sumrua.25.111
b492bccd-1226-4144-bbfd-29f374abd7aa
名前 / ファイル ライセンス アクション
oka2013.pdf oka2013.pdf (8.9 MB)
Item type 紀要論文 / Departmental Bulletin Paper(1)
公開日 2015-05-11
タイトル
タイトル 北海道厚真川下流域の後期更新世~完新世の古環境変遷
その他のタイトル
その他のタイトル Environmental analysis of Late Pleistocene to Holocene drilling core in the lowland along the downstream of Atsuma River, Hokkaido, Japan
著者 岡, 孝雄

× 岡, 孝雄

WEKO 83938

岡, 孝雄

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近藤, 務

× 近藤, 務

WEKO 83939

近藤, 務

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中村, 俊夫

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WEKO 83940

中村, 俊夫

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星野, フサ

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WEKO 83941

星野, フサ

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安井, 賢

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WEKO 83942

安井, 賢

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井島, 行夫

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WEKO 83943

井島, 行夫

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関根, 達夫

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WEKO 83944

関根, 達夫

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米道, 博

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WEKO 83945

米道, 博

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宿田, 浩司

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WEKO 83946

宿田, 浩司

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山崎, 芳樹

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WEKO 83947

山崎, 芳樹

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乾, 哲也

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WEKO 83948

乾, 哲也

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奈良, 智法

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WEKO 83949

奈良, 智法

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Oka, Takao

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WEKO 83950

Oka, Takao

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Kondou, Tsutomu

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WEKO 83951

Kondou, Tsutomu

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Nakamura, Toshio

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WEKO 83952

Nakamura, Toshio

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Hoshino, Fusa

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WEKO 83953

Hoshino, Fusa

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Yasui, Satoshi

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WEKO 83954

Yasui, Satoshi

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Ijima, Yukio

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WEKO 83955

Ijima, Yukio

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Sekine, Tatsuo

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WEKO 83956

Sekine, Tatsuo

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Yonemichi, Hiroshi

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WEKO 83957

Yonemichi, Hiroshi

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Shukuda, Koji

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WEKO 83958

Shukuda, Koji

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Yamazaki, Yoshiki

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WEKO 83959

Yamazaki, Yoshiki

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Inui, Tetsuya

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WEKO 83960

Inui, Tetsuya

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Nara, Tomonori

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WEKO 83961

Nara, Tomonori

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キーワード
主題Scheme Other
主題 Atsuma River
キーワード
主題Scheme Other
主題 Pollen Analysis
キーワード
主題Scheme Other
主題 Diatom Analysis
キーワード
主題Scheme Other
主題 Jomon-Tansgression
キーワード
主題Scheme Other
主題 Tephra
抄録
内容記述 Two drilling cores (46 meters core of AZK-1 and 25 meters core of S60Kー1), in the lowland along the downstream of Atsuma River, southern Hokkaido, were investigated based on lithologic observation, microbiostratigraphy (pollen and diatom), tephrochronology and radiocarbon dating (14C dating;AMS). AZK-1 drilling hole, located in the river mouth area of Atsuma, is composed of AZK-1-1(last inter-glacial stage deposits), AZK-1-2 (buried terrace deposits, fluvial), AZK-1-3 (upper part of so-called “Chuseki formation") and AZK-1-4 (artificial bank) upward stratigraphically. 60SK-1 drilling hole, located in the town area of Kamiatsuma, is divided thirteen lithological units. All units of 60SK-1 drilling hole are compose the upper part of so-called “Chuseki formation". Diatom analysis is very useful for the study of “Chuseki formation" under the influence of sea water especially. The stage of brackish water of AZK-1 core is post-era, while one of 60SK-1 core is about five thousand years ago.
内容記述タイプ Abstract
内容記述
内容記述 名古屋大学年代測定総合研究センターシンポジウム報告
内容記述タイプ Other
出版者
出版者 名古屋大学年代測定資料研究センター
言語
言語 jpn
資源タイプ
資源 http://purl.org/coar/resource_type/c_6501
タイプ departmental bulletin paper
ID登録
ID登録 10.18999/sumrua.25.111
ID登録タイプ JaLC
書誌情報 名古屋大学加速器質量分析計業績報告書

巻 25, p. 111-124, 発行日 2014-03
著者版フラグ
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