CLAY MINERALOGICAL APPROACH TO THE SLIP-SURFACE FORMATION IN THE O'DOKORO LANDSLIDE, NIIGATA, CENTRAL JAPAN

Samples were collected form the O'dokoro landslide in Niigata prefecture for the mineralogical analysis. The O'dokoro landslide occurs in the sheared belts, located 5 km west from the Itoigawa-Shizuoka Tectonic Line and is positioned in the serpentinite melange. Lamellar serpentinite sampl...

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Veröffentlicht in:Clay Science 2000, Vol.11(2), pp.107-113
Hauptverfasser: EGASHIRA, KAZUHIKO, MATSUO, KOUICHI, GIBO, SEIICHI, NAKAMURA, SHINYA, ZHOU, YAMING, INOUE, HIDEMASA, SASAKI, KEIZO
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Sprache:eng
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