Abstract
6.5). They show a clear tendency for higher static stress drops than shallow events, and for magnitudes above 7, average stress drops exceeding 10 MPa may be expected. These results are of particular significance for seismic hazard studies, and specifically for the estimation of future strong motions.
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Gusev, A., Radulian, M., Rizescu, M., & Panza, G. F. (2002). Source scaling of intermediate-depth Vrancea earthquakes. Geophysical Journal International, 151(3), 879–889. https://doi.org/10.1046/j.1365-246X.2002.01816.x
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