A particular sequence of crustal earthquakes (h < 10 km, M(L) < 5.1) o
ccurred in the southwestern extremity of the Eastern Carpathian are be
nd (Sinaia region) starting on May 4, 1993. The main shock (M(L) 5.1)
occurred on May 23 after significant 20-day foreshock activity. The fi
rst locations delineate an epicentral area of approximately 225 km(2),
elongated in a NW-SE direction, which agrees with the fault plane sol
ution for the main shock. The digital recordings of the Romanian telem
etered network are analyzed in order to estimate source parameters and
to investigate scaling relations. An empirical deconvolution techniqu
e and the spectral ratio method are used for this purpose. The main re
sults, such as (1) the departure from a M(0)(1/3) scaling of the sourc
e radius as a function of the seismic moment, (2) the scaling of the p
eak velocity parameter as a function of local magnitude and (3) the sc
aling of the dynamic stress drop with earthquake size, are interpreted
in terms of an inhomogeneous source model.