Mechanism of creep movement caused by landslide activity and underground erosion in crystalline schist, Shikoku Island, southwestern Japan

Author:

Furuya G.,Sassa K.,Hiura H.,Fukuoka H.

Publisher

Elsevier BV

Subject

Geology,Geotechnical Engineering and Engineering Geology

Reference28 articles.

1. Remarks on landslides in crystalline schist areas, Tokushima Prefecture, Shikoku;Ando;Bull. Geol. Surv. Japan,1970

2. Baumer, A., 1988. Three rock slides in the southern Swiss Alps. In: Bonnard, C. (Ed.), Proc. 5th International Symp. on Landslides, Lausanne, vol. 2, Balkema, Rotterdam, pp. 1307–1311.

3. Bonnard, C., 1983. Determination of slow landslide activity by multidisciplinary measurement techniques. In: Kovari, K. (Ed.), International Symp. on Field Measurements in Geomechanics, Zurich, Balkema, Rotterdam, pp. 619–638.

4. Mass rock creep of crystalline schist (Part 1): the relationship between geological structures and landslide topographies in the Sambagawa terrain in the Kanto mountainous land;Chigira;J. Jap. Soc. Eng. Geol.,1984

5. Mass rock creep of crystalline schist (Part 2): minor structures formed by mass rock creep;Chigira;J. Jap. Soc. Eng. Geol.,1985

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