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- W2019966053 abstract "The geology of the Yasukuni landslide area consists mainly of tuffaceous clastic rocks and acidic volcaniclastic rocks of the Upper Miocene Ikutawara Formation, in which an interstratified illite/smectite minerals zone exists, formed by hydrothermal alteration related to the 8.1-7.7 Ma Ryuo hydrothermal system. The slide clays and debris contain large amounts of interstratified illite/smectite minerals. The occurrence of the Yasukuni slide is strongly related to the unstable nature of the interstratified illite/smectite minerals zone, the bulk of which is swelling clay mineral. This fact is useful in evaluating landslide risk and creating a hazard map of such slides in ancient and active hydrothermal fields." @default.
- W2019966053 created "2016-06-24" @default.
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- W2019966053 date "2001-01-01" @default.
- W2019966053 modified "2023-10-04" @default.
- W2019966053 title "The Relationship between the Yasukuni Slide and a Hydrothermal Interstratified Illite/Smectite Minerals Zone" @default.
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- W2019966053 doi "https://doi.org/10.3313/jls1964.37.4_1" @default.
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