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In seismology an earthquake source is described in terms of a fault with a particular rupture size. In particular, the descrip tion and simulation of strong ground motion are very important not only for problems directly relevant to earthquake engineering, but also to the frac ture mechanics of earthquake faulting.
In seismology an earthquake source is described in terms of a fault with a particular rupture size. In particular, the descrip tion and simulation of strong ground motion are very important not only for problems directly relevant to earthquake engineering, but also to the frac ture mechanics of earthquake faulting.
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