A large number of earthquakes have been modelled in detail using seismological, geological and ')Y1c O
geodetic information. Several common traits have been found for earthquakes kinematics at ZKM@ U?PK
periods longer than 3s. At these frequencies, all large earthquakes (M>7) appear complex with #$}A$ sm
highly variable slip, and propagate with rupture velocities close to about 80 % of the shear wave 5=8t<v1Bn
speed. Starting from these kinematic inversions, it is possible to use numerical wave propagation !lBK!'0
models in order to estimate the complete radiated field including near and far field effects. ]zn 3nhBI
Radiation can be separated into two main components: a near field term responsible for the socalled as@?
Kv
fling steps due to permanent, geodetic offsets; and the far field that produces pulse like %AmyT
motions. Using seismological scaling relations it is possible to explain the main features of i1*0'x
displacement spectra using classical seismological models at long periods. Seismic simulations
{BgJ=0g?
may now be extended to the frequencies up to a few Hz by means of dynamic rupture propagation, yJ ;Qe_up
where rupture is simulated starting from the kinematic models. In this talk I will review the main g Mp' S
results obtained so far and the new avenues of research that have been opened thanks to new near 3 rR 1/\
field earthquake data and the ability to simulate increasingly complex and realistic seismic ` $q0fTz
ruptures in a computer.
