Reconsideration of the subdivision of "alluvium' in enclosed coastal seas - the example of Osaka Bay

Yoshio Inouchi

研究成果: Chapter

1 被引用数 (Scopus)

抄録

Unconsolidated muddy sediment, which forms the upper and middle parts of "Alluvium' in Japanese enclosed coastal seas, cannot be stratigraphically subdivided. The sandy part near the channel area and the muddy parts in the central bay and the area far away from the channels (both on the bottom surface) are in the relation of a contemporaneous heterotopic facies. The most obvious reflector in the acoustic record is better understood as the boundary between the upper and middle muddy "Alluvium' and the underlying "lower Alluvium'. -from English summary

本文言語English
ホスト出版物のタイトルQuaternary Research (Tokyo)
ページ405-416
ページ数12
29
5
出版ステータスPublished - 1990
外部発表はい

ASJC Scopus subject areas

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

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