How seismic velocity acts across the deformed sediments?
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Relationships between depth–average flow velocity and (A) the transported sediment volume for runs 11–14; (B) the observed number of grainflows for runs 11– 14, and; (C) the number of ripples superimposed on dunes at any time for runs 2 to 5. The data points indicate average numbers, the error bars indicate the standard deviation. The number of ripples on dunes decreases with increasing flow velocity.
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When earthquakes occur, a buildings undergoes dynamic motion. This is because the building is subjected to inertia forces that act in opposite direction to the acceleration of earthquake excitations. These inertia forces, called seismic loads, are usually dealt with by assuming forces external to the building.
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