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- W2334960015 abstract "On the distinction between the landslide and the landslide, there is no defi, nited theory in our country, yet. Generally, in case of the landslide, clay substances invitate the landslide movement. There are many landslide districts in Niigata Pref. Above all, landslide frequently occurs in Gendozi district, Nakakubigun. The geology in this district consists of the Teradomari formation and its chief is black shale, and combine the tuffaceous clay and sandy beds. The result of studies on the habits of tuffaceous clay using X-ray analysis, chemical analysis and colouring method, the fact is cleared up that this is the bentonitic clay containing montmorillonite as chief clay mineral. Consequently, I guessed montmorillonite was swelled by ground water and underground water and the bed became unstable to cause the landslide." @default.
- W2334960015 created "2016-06-24" @default.
- W2334960015 creator A5021819986 @default.
- W2334960015 date "1962-01-01" @default.
- W2334960015 modified "2023-09-25" @default.
- W2334960015 title "Clay minerals on the landslide disrict in Arai subrub, Niigata prefecture" @default.
- W2334960015 doi "https://doi.org/10.2465/ganko1941.48.235" @default.
- W2334960015 hasPublicationYear "1962" @default.
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