結晶片岩の岩盤クリープ(その1) : 関東山地三波川帯の地質構造と地すべり地形との関連 Mass Rock Creep of Crystalline Schist (Part 1) : The Relationship between Geologic Structures and Landslide Topographies in the Sambagawa Terrain in the Kanto Mountainous Land

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著者

抄録

Geological and geomorphological invesigation was performed in the Kanto mountainous land to study the relationship between geology and landslide topographies in the Sambagawa terrain where crystalline schist is distributed. Landslide topographies were found to be abundant in pelitic and basic schist ranges and scarce in siliceous schist, psammitic schist, and massive basic rock ranges. It was elucidated that the landslide topographies have the size and the moving direction, both are controlled by the attitude of the basement rocks. The landslide topographies that show the movement about parallel with the dip direction of the basement rocks exceed the other landslide topographies in their number and in their size.

収録刊行物

  • 応用地質

    応用地質 25(4), 182-194, 1984-12-30

    一般社団法人日本応用地質学会

被引用文献:  10件中 1-10件 を表示

各種コード

  • NII論文ID(NAID)
    110003356297
  • NII書誌ID(NCID)
    AN00026635
  • 本文言語コード
    JPN
  • 資料種別
    雑誌論文
  • ISSN
    02867737
  • NDL 記事登録ID
    3016218
  • NDL 刊行物分類
    ME61(地質・地史)
  • NDL 雑誌分類
    ZM49(科学技術--地球科学--地質)
  • NDL 請求記号
    Z15-263
  • データ提供元
    CJP引用  NDL  NII-ELS  J-STAGE 
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