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  1. 040 理学部
  2. 0401 学術論文

Shimanto geosyncline and Kuroshio paleoland

http://hdl.handle.net/10091/12032
e680cd31-7649-4415-b23d-c33d98966d18
名前 / ファイル ライセンス アクション
Shimanto_geosyncline_Kuroshio_paleoland.pdf Shimanto_geosyncline_Kuroshio_paleoland.pdf (832.8 kB)
Item type 学術雑誌論文 / Journal Article(1)
公開日 2011-03-16
タイトル
言語 en
タイトル Shimanto geosyncline and Kuroshio paleoland
言語
言語 eng
資源タイプ
資源 http://purl.org/coar/resource_type/c_6501
タイプ journal article
著者 Harata, T

× Harata, T

WEKO 36346

Harata, T

Search repository
Hisatomi, K

× Hisatomi, K

WEKO 36347

Hisatomi, K

Search repository
Kumon, F

× Kumon, F

WEKO 36348

Kumon, F

Search repository
Nakazawa, K

× Nakazawa, K

WEKO 36349

Nakazawa, K

Search repository
Tateishi, M

× Tateishi, M

WEKO 36350

Tateishi, M

Search repository
Suzuki, H

× Suzuki, H

WEKO 36351

Suzuki, H

Search repository
Tokuoka, T

× Tokuoka, T

WEKO 36352

Tokuoka, T

Search repository
信州大学研究者総覧へのリンク
氏名 Kumon, F
URL http://soar-rd.shinshu-u.ac.jp/profile/ja.ZUchOUkh.html
出版者
出版者 Seismological Society of Japan
引用
内容記述タイプ Other
内容記述 Journal of Physics of the Earth. 26(suppl):357-366 (1978)
書誌情報 Journal of Physics of the Earth

巻 26, 号 suppl, p. 357-366, 発行日 1978
抄録
内容記述タイプ Abstract
内容記述 The late Mesozoic to early Neogene geosyncline in the Outer zone of Southwest Japan has been studied in detail in the Kii Peninsula by the Research Group for the Shimanto Geosyncline. The existence of the Kuroshio Paleoland to the south of the geosyncline was inferred by various sedimentologic evidences. The Shimanto belt in the Kii Peninsula is divided from north to south into three zones of Cretaceous, Eocene and Oligocene to lower Miocene. In these belts thick geosynclinal sediments were accumulated showing coarsening upward. The southward migration of the basin occurred in Cretaceous/Eocene, Eocene/Oligocene, and in early Miocene. In the present paper the reconstruction of paleogeography of the Shimanto geosyncline was attempted and the Kuroshio Paleoland was discussed in relation to the geohistory of the Philippine Sea. In spite of the detailed geologic survey in the Kii Peninsula there is no evidence of large exotic blocks nor tectonic mélanges, and this does not support the plate tectonic model ofthe Pacific-type orogeny for the Shimanto belt.
資源タイプ(コンテンツの種類)
内容記述タイプ Other
内容記述 Article
ISSN
収録物識別子タイプ PISSN
収録物識別子 0022-3743
書誌レコードID
収録物識別子タイプ NCID
収録物識別子 AA00704960
DOI
関連タイプ isIdenticalTo
関連識別子
識別子タイプ DOI
関連識別子 https://doi.org/10.4294/jpe1952.26.Supplement_S357
出版タイプ
出版タイプ VoR
出版タイプResource http://purl.org/coar/version/c_970fb48d4fbd8a85
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