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  1. B100 理学部/理学研究科
  2. B100b 紀要
  3. The Journal of earth and planetary sciences
  4. 53

Lithology and radiolarian age of the Hidakagawa Sub-belt of the Shimanto Belt in the western Kii Peninsula, southwest-Japan

https://doi.org/10.18999/joueps.53.1
https://doi.org/10.18999/joueps.53.1
ebf46126-b8bf-47f4-8aae-dfd553c857fa
名前 / ファイル ライセンス アクション
KJ00004741137.pdf KJ00004741137.pdf (3.1 MB)
Item type 紀要論文 / Departmental Bulletin Paper(1)
公開日 2008-02-18
タイトル
タイトル Lithology and radiolarian age of the Hidakagawa Sub-belt of the Shimanto Belt in the western Kii Peninsula, southwest-Japan
言語 en
著者 TOKIWA, Tetsuya

× TOKIWA, Tetsuya

WEKO 19964

en TOKIWA, Tetsuya

Search repository
UEHARA, Hirohito

× UEHARA, Hirohito

WEKO 19965

en UEHARA, Hirohito

Search repository
WIN, Kyaw Soe

× WIN, Kyaw Soe

WEKO 19966

en WIN, Kyaw Soe

Search repository
TAKEUCHI, Makoto

× TAKEUCHI, Makoto

WEKO 19967

en TAKEUCHI, Makoto

Search repository
アクセス権
アクセス権 open access
アクセス権URI http://purl.org/coar/access_right/c_abf2
抄録
内容記述 This study focuses on the lithology and radiolarian age of the Hidakagawa Sub-belt in the Shimanto Belt, Southwest Japan. The rocks of the Hidakagawa Sub-belt are divided into the Unit 1 consisting of only terrigenous deposits and Unit 2 consisting of terrigenous deposits with chert and red shale. The Unit 1 is subdivided into the Sub-unit 1A composed largely of thick-bedded sandstone with unknown age and Sub-unit 1B composed largely of late Albian to late Cenomanian sandstone-rich alternating beds of sandstone and shale. The Unit 2 is subdivided into the Sub-unit 2A composed largely of early Coniacian shale-rich alternating beds of sandstone and shale with mixed rock including sandstone, chert, and red shale, and Sub-unit 2B composed largely of latest Santonian to early Campanian thick-bedded sandstone with mixed rock including sandstone and red shale.<br/> On this basis of lithology, radiolarian age, and stratigraphic position, the Sub-units 1A and 1B are correlated to the Y3 and Y1 Members of Yukawa Formation in the central Kii Peninsula, and they can be correlated with the Ogui and Nagasaki Sub-units of Yukawa Unit in the coastal area of Kii Peninsula, respectively. The Sub-unit 2A and 2B correspond to the M1 and M2b Members of Miyama Formation in the central Kii Peninsula, and these sub-units can be correlated with the Karakozaki and Chidenohana Sub-units of Miyama Unit in the coastal area of Kii Peninsula, respectively.
言語 en
内容記述タイプ Abstract
内容記述
内容記述 国立情報学研究所で電子化したコンテンツを使用している。
言語 ja
内容記述タイプ Other
出版者
言語 en
出版者 Dept. of Earth and Planetary Sciences, Nagoya University
言語
言語 eng
資源タイプ
資源 http://purl.org/coar/resource_type/c_6501
タイプ departmental bulletin paper
出版タイプ
出版タイプ VoR
出版タイプResource http://purl.org/coar/version/c_970fb48d4fbd8a85
ID登録
ID登録 10.18999/joueps.53.1
ID登録タイプ JaLC
ISSN(print)
収録物識別子タイプ PISSN
収録物識別子 0919-875X
書誌情報 en : The Journal of Earth and Planetary Sciences, Nagoya University

巻 53, p. 1-14, 発行日 2006
フォーマット
application/pdf
著者版フラグ
値 publisher
URI
識別子 http://hdl.handle.net/2237/9420
識別子タイプ HDL
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