Titlebook: Natural and Man-Made Hazards; Proceedings of the I M. I. El-Sabh,T. S. Murty Conference proceedings 1988 D. Reidel Publishing Company, Dord

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The 1985 Mexico Earthquakeof strong ground motion in sedimentary basins; (b) the enhanced transmission of low-frequency seismic energy from the subduction coast inland; and (c) the unexpected behavior of tall buildings on soft saturated sediments under low-frequency, harmonic oscillations. A critical discussion of available

高原

Seismic Ground Motion and Damage Caused by Large Earthquakes in Nagoya, Japanated for three earthquakes: the Nobi earthquake of 1891, the Tonankai earthquake of 1944 and the Mikawa earthquake of 1945. On the other hand, damage ratios to wooden houses in each mesh area due to these earthquakes were obtained by rearranging original data. From the comparison of seismic ground m

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A New Approach for a Quick Estimation of the Seismic Moment, Magnitude Mm? the rapid determination of the seismic moment, by simply using the amplitude of the long periods of the vertical component of Rayleigh waves; we define experimentally, a Magnitude scale Mm, directly proportional to the decimal logarithm of the moment and to the energy released by the earthquakes. T

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The Effects of Seismic Activity on the Soils of the Charlevoix Area—Quebec, Canada but the marine deposits laid down since the end of the last glacial episode (10 000 years before now) “witnessed” the seismic activity that affected them. Intraformational deformation, usually attributed in Quebec to glacial processes, may also result from seismic activity. A study by Chagnon and L

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Risk Assessment of the Tsunami Hazard vast expanses of our planet with an intensity and suddenness comparable to that of large earthquakes. But even the effects of such large earthquakes are relatively localized compared to the devastating impact that their offsprings, tsunamis, can have, often across an entire ocean..When the tsunami