Source parameters of small events using constrained deconvolution with empirical Green's functions

An iterative and constrained deconvolution technique, called projected Land weber deconvolution (PLD), is applied to a local earthquake data set record ed in the southwestern Alps (NW Italy) in order to estimate the relative so urce time function (RSTF) of the events. The magnitude range analysed is 1. 4 < M-L < 4.3. The smallest events (M-L < 2.0) are used as empirical Green' s functions (EGF) to deconvolve the larger earthquakes. The crucial choice of appropriate EGF is tackled using high-precision relative locations. Resu lts demonstrate that PLD successfully overcomes the instability effects of the deconvolution process and provides stable and reliable RSTFs. Moreover, this method allows us to obtain an objective determination of the duration of the RSTF, which is essential to estimate correctly the source size. Com bining the information inferred from both RSTFs and displacement spectra, s ource parameters are computed for all the events. We obtain seismic moments ranging from 2.9 x 10(11) to 3.1 x 10(14) N m and source radii between 70 and 700 m. Taking the instrumental limits into account, no breakdown in con stant stress drop scaling is seen in our estimates.