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北海道東部、常呂帯湧別層群向遠軽層の渦鞭毛藻化石年代(前期始新世)とその意義
http://hdl.handle.net/10191/17798
http://hdl.handle.net/10191/17798e22cbbc4-ae19-4ae2-bd93-078d20843dd1
名前 / ファイル | ライセンス | アクション |
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ZC_104(11)_808-811.pdf (993.5 kB)
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Item type | 学術雑誌論文 / Journal Article(1) | |||||
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公開日 | 2012-04-11 | |||||
タイトル | ||||||
タイトル | 北海道東部、常呂帯湧別層群向遠軽層の渦鞭毛藻化石年代(前期始新世)とその意義 | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | 北海道東部、常呂帯湧別層群向遠軽層の渦鞭毛藻化石年代(前期始新世)とその意義 | |||||
言語 | ||||||
言語 | jpn | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | Hokkaido | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | Tokoro Belt | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | Yubetsu Group | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | dinoflagellate cysts | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | Eocene | |||||
資源タイプ | ||||||
資源 | http://purl.org/coar/resource_type/c_6501 | |||||
タイプ | journal article | |||||
その他のタイトル | ||||||
その他のタイトル | Tectonic implications of Early Eocene dinoflagellate cysts from the Mukai-engaru Formation of the Yubetsu Group, Tokoro Belt, eastern Hokkaido, Japan | |||||
著者 |
栗田, 裕司
× 栗田, 裕司× 田近, 淳 |
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著者別名 | ||||||
識別子 | 41605 | |||||
識別子Scheme | WEKO | |||||
姓名 | Kurita, Hiroshi | |||||
著者別名 | ||||||
識別子 | 41606 | |||||
識別子Scheme | WEKO | |||||
姓名 | Tajika, Jun | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | A diverse marine dinoflagellate cyst assemblage of an Early Eocene age was recovered from the Mukai-engaru Formation of the Yubetsu Group, Tokoro Belt, eastern Hokkaido, Japan, from which no fossil occurrence was previously recorded. The Early Eocene age is the youngest known age of the group and provides two geochronological constraints significant to the regional tectonic history. First, the age of the formation agrees well with the accretionary prism model proposed for the Yubetsu Group, since the age was determined in the probable youngest part of the whole group in the model. Second, the present age determination denotes that the eastward accretion-subduction to the Paleo-Kuril Arc or the Okhotsk Block was still active in the Early Eocene. The observed geochronological range of the Yubetsu Group is well paralleled by that of the Hidaka Supergroup in the Hidaka Belt to the west, which implies a temporal similarity between the two confronting convergent margins. | |||||
書誌情報 |
地質学雑誌 en : 地質学雑誌 巻 104, 号 11, p. 808-811, 発行日 1998-11 |
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出版者 | ||||||
出版者 | 日本地質学会 | |||||
ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 00167630 | |||||
書誌レコードID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AN00141768 | |||||
著者版フラグ | ||||||
値 | publisher |