Cretaceou biostratigraphy and ammonites in Hokkaido, Japan.

H. Hirano

研究成果: Chapter

4 引用 (Scopus)

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The Cretaceous sediments of Hokkaido are composed of miogeosynclinal and deltaic sediments from the Aptian to the Maastrichtian, distributed in two belts westward of the paired metamorphic belts. The ammonite fauna belongs to the Pacific- Tethyan realm and is dominated by off-shore forms. Correlation with the European standard by ammonites, inocerami, foraminifers, radiolarians and nannoplankton has been undertaken concurrently in the three districts. -from Author

元の言語English
ホスト出版物のタイトルProceedings Geologists' Association
ページ213-223
ページ数11
93
エディション2
出版物ステータスPublished - 1982

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biostratigraphy
nanoplankton
ammonite
Aptian
Maastrichtian
sediment
foraminifera
fauna
Cretaceous
European standard

ASJC Scopus subject areas

  • Earth and Planetary Sciences(all)
  • Environmental Science(all)

これを引用

Hirano, H. (1982). Cretaceou biostratigraphy and ammonites in Hokkaido, Japan.Proceedings Geologists' Association (2 版, 巻 93, pp. 213-223)

Cretaceou biostratigraphy and ammonites in Hokkaido, Japan. / Hirano, H.

Proceedings Geologists' Association. 巻 93 2. 編 1982. p. 213-223.

研究成果: Chapter

Hirano, H 1982, Cretaceou biostratigraphy and ammonites in Hokkaido, Japan.Proceedings Geologists' Association. 2 Edn, 巻. 93, pp. 213-223.
Hirano H. Cretaceou biostratigraphy and ammonites in Hokkaido, Japan. : Proceedings Geologists' Association. 2 版 巻 93. 1982. p. 213-223
Hirano, H. / Cretaceou biostratigraphy and ammonites in Hokkaido, Japan. Proceedings Geologists' Association. 巻 93 2. 版 1982. pp. 213-223
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