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[2]
Trifunac M.D., Preliminary analysis of the peaks of strong earthquake ground motion—dependence of peaks on earthquake magnitude, epicentral distance and the recording site conditions, Bull. Seism. Soc. Am., 65, pp. 189-219, (1976)
[3]
Trifunac M.D., Preliminary empirical model for scaling Fourier amplitude spectra of strong ground acceleration in terms of earthquake magnitude, source to station distance and recording site conditions, Bull. Seism. Soc. Am., 66, pp. 1343-1373, (1976)
[4]
Trifunac M.D., Brady A.G., On the correlation of seismic intensity scales with the peaks of recorded strong ground motion, Bull. Seism. Soc. Am., 65, pp. 129-162, (1975)
[5]
Barosh P.J., (1969)
[6]
Trifunac M.D., pp. 2-359, (1977)
[7]
Trifunac M.D., pp. 10-25, (1977)
[8]
Trifunac M.D., Anderson J.G., (1977)
[9]
Wong H.L., Trifunac M.D., A note on an instrumental comparison of the Modified Mercalli (MMI) and the Japanese Meteorological Agency (JMA) intensity scales, based on computed peak accelerations, Earthqu. Eng. Struct. Dyn., 7, pp. 75-83, (1979)
[10]
Trifunac M.D., A note on the range of peak amplitudes of recorded accelerations, velocities and displacements with respect to the Modified Mercalli Intensity, Earthquake Notes, 47, pp. 9-24, (1976)