東北地方の新第三紀・泥岩層における褶曲及び断層構造の成因と地すべりとの関連性

DOI Web Site 被引用文献6件 参考文献14件

書誌事項

タイトル別名
  • Study of the Relationship between Landslides and the Origin of Fold and Fault Structures in the Neogene mudstone layers of the Tohoku District
  • トウホク チホウ ノ シンダイ3キ デイガンソウ ニ オケル シュウキョク オヨビ ダンソウ コウゾウ ノ セイイン ト ヂスベリ ト ノ カンレンセイ

この論文をさがす

抄録

Up to now, the folds, faults, etc., found in the areas of frequent landslide occurrence in the “green-tuff” region of the Tohoku district have been considered to originate in the diastrophism.<BR>A great deal of research has been conducted into geological structures-such as folds and faults-that are caused by various factors: the bedrock movement following the ground upheaval continuing to the present day; the gravity slides that occurred in the mudstone sedimentation on the ocean floor; bedrock deformation due to the large-scale original rock slides that occurred frequently in Quaternary; and so on.<BR>We have already reported the case of the western area of the Ou mountains in detail. In this report, we will further describe the fold and fault structures and landslides in the Dewa Hill areas, the fold structure and landslides in the surrounding granite areas of the Tohoku district, and the relationship between some aspect of fault structures and landslides.

収録刊行物

  • 地すべり

    地すべり 33 (1), 20-28_1, 1996

    公益社団法人 日本地すべり学会

被引用文献 (6)*注記

もっと見る

参考文献 (14)*注記

もっと見る

キーワード

詳細情報 詳細情報について

問題の指摘

ページトップへ