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

DOI 5 Citations

Abstract

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.

Journal

  • Landslides

    Landslides 26 (3), 10-18, 1989

    The Japan Landslide Society

Citations (5)*help

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Details 詳細情報について

  • CRID
    1390282679521954816
  • NII Article ID
    130001009025
  • DOI
    10.3313/jls1964.26.3_10
  • ISSN
    18843956
    02852926
  • Text Lang
    en
  • Data Source
    • JaLC
    • Crossref
    • CiNii Articles
  • Abstract License Flag
    Disallowed

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