Titlebook: International Small and Medium-Sized Enterprises; Internationalization Edith Olejnik Book 2014 Springer Fachmedien Wiesbaden 2014 Internati

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and rotational slides occurred on the cataclinal and orthoclinal slope, respectively. It had been thought that mechanism of those landslides was not so complicated because of the simple structure. During the excavation for the countermeasure of those landslides, however, a vertical fault, which loo

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Edith Olejnikip slopes and anti-dip slopes have significant PGA amplifications at the upper top region. Results of numerical simulation and fracture mechanics based calculation show that failure development parts of the dip slopes and anti-dip slopes are different.

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Edith Olejnik?km away. Flow of unconsolidated volcanic sediment and rock failures of consolidated bedrock occurred at locations 200–300?km away. These indicate that magnitude 8 is the line of demarcation at which the relationship between the distance from the epicenter to landslide sites and the movement types c

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Edith Olejniksee to what extent natural rubber bearings could be used to protect buildings from earthquakes. Very soon after this meeting, we were able to do such a test using a 20-ton model and hand-made isolators. The eady tests were very promising. Accordingly, a further set of tests was done with a more real

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see to what extent natural rubber bearings could be used to protect buildings from earthquakes. Very soon after this meeting, we were able to do such a test using a 20-ton model and hand-made isolators. The eady tests were very promising. Accordingly, a further set of tests was done with a more real

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ones occurred with many small-scale ones by the 2007 Mid-Niigata Offshore Earthquake in spite of their similar geology and topography [landslide-scale with apparent volume (the Japan Landslide Society, .); small-scale: 10.–10. m., middle-scale: 10.–10. m., large-scale: 10.–10.m.]. Some of them, howe

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Edith Olejnikgy, geology, and types of movement at the sites of earthquake landslides including those of the 2011 Tohoku Earthquake. Earthquake landslides show common movement types with similar geological properties. They are (1) translational slides in ridges and cuestas with Tertiary–Quaternary well-bedded se