日本海側に発達する最上部新生界の石灰質微化石層序 I  新潟地域

書誌事項

タイトル別名
  • Calcareous microfossil biostratigraphy of the uppermost cenozoic formations distributed in the coast of the Japan Sea. Part 1 Niigata area.
  • Part 1: Niigata Area
  • その1: 新潟地域
公開日
1987
DOI
  • 10.3720/japt.52.231
公開者
石油技術協会

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説明

Eleven calcareous nannofossil biohorizons are recognized in the Quaternary sequences at six sites drilled in the Northeast Atlantic Ocean during DSDP-IPOD Leg 94. Correlation of those biohorizons with the magnetostratigraphy is established, and ages of all datums are estimated by interpolation between magnetic reversals (TAKAYAMA and SATO, 1986). The calcareous nannofossil and the foraminiferal assemblages of the Nishiyama and the Haizume formations distributed in the Oginojo area, near the type locality of the Haizume Formation, Niigata district are described, and five calcareous nannofossil biohorizons are recognized. Based on the above mentioned results of DSDP-IPOD Leg 94, the middle Nishiyama through the Haizume formations are Pleistocene in age and can be correlated with the interval between the Olduvai and the Jaramillo events of the magnetostratigraphy. This age assignment agrees neither with the magnetostratigraphic interpretations (YOSHIKOSHI, 1983) nor with the fission track datings (MURAMATSU, 1983), which were undertaken in the Oguni area 25 kilometers south of the present area.

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詳細情報 詳細情報について

  • CRID
    1390282679037613440
  • NII論文ID
    130003921963
  • DOI
    10.3720/japt.52.231
  • ISSN
    18814131
    03709868
    http://id.crossref.org/issn/03709868
  • 本文言語コード
    ja
  • データソース種別
    • JaLC
    • Crossref
    • CiNii Articles
  • 抄録ライセンスフラグ
    使用不可

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