Cretaceou biostratigraphy and ammonites in Hokkaido, Japan.

H. Hirano

Research output: Chapter in Book/Report/Conference proceedingChapter

4 Citations (Scopus)

Abstract

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

Original languageEnglish
Title of host publicationProceedings Geologists' Association
Pages213-223
Number of pages11
Volume93
Edition2
Publication statusPublished - 1982

Fingerprint

biostratigraphy
nanoplankton
ammonite
Aptian
Maastrichtian
sediment
foraminifera
fauna
Cretaceous
European standard

ASJC Scopus subject areas

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

Cite this

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

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

Proceedings Geologists' Association. Vol. 93 2. ed. 1982. p. 213-223.

Research output: Chapter in Book/Report/Conference proceedingChapter

Hirano, H 1982, Cretaceou biostratigraphy and ammonites in Hokkaido, Japan. in Proceedings Geologists' Association. 2 edn, vol. 93, pp. 213-223.
Hirano H. Cretaceou biostratigraphy and ammonites in Hokkaido, Japan. In Proceedings Geologists' Association. 2 ed. Vol. 93. 1982. p. 213-223
Hirano, H. / Cretaceou biostratigraphy and ammonites in Hokkaido, Japan. Proceedings Geologists' Association. Vol. 93 2. ed. 1982. pp. 213-223
@inbook{441b81f3ea974f20ba46afd83f02e21b,
title = "Cretaceou biostratigraphy and ammonites in Hokkaido, Japan.",
abstract = "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",
author = "H. Hirano",
year = "1982",
language = "English",
volume = "93",
pages = "213--223",
booktitle = "Proceedings Geologists' Association",
edition = "2",

}

TY - CHAP

T1 - Cretaceou biostratigraphy and ammonites in Hokkaido, Japan.

AU - Hirano, H.

PY - 1982

Y1 - 1982

N2 - 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

AB - 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

UR - http://www.scopus.com/inward/record.url?scp=0019925675&partnerID=8YFLogxK

UR - http://www.scopus.com/inward/citedby.url?scp=0019925675&partnerID=8YFLogxK

M3 - Chapter

VL - 93

SP - 213

EP - 223

BT - Proceedings Geologists' Association

ER -