Gravitational creep folds in the Izumi Group of the Izumi Mountains, southwest Japan.

DOI 被引用文献5件

抄録

Because of a high ductility contrast between sandstone and mudstone in the uppermost Cretaceous Izumi Group, gravitational force has led to the development of symmetric and asymmetric folds in beds within a few meters below the ground surface in many quarry scars . These gravitational creep folds has taken place during two or three decades after excavation.

収録刊行物

  • 地すべり

    地すべり 26 (3), 10-18, 1989

    公益社団法人 日本地すべり学会

被引用文献 (5)*注記

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詳細情報 詳細情報について

  • CRID
    1390282679521954816
  • NII論文ID
    130001009025
  • DOI
    10.3313/jls1964.26.3_10
  • ISSN
    18843956
    02852926
  • 本文言語コード
    en
  • 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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