MODELING OF ENERGY AMPLIFICATION RECORDED WITHIN GREATER LOS-ANGELES USING IRREGULAR STRUCTURE

We have investigated energy amplification observed within Greater Los Angeles basin by analyzing regional waveforms recorded from several Ne vada Test Site (NTS) nuclear explosions. Although the stations are loc ated nearly at the same azimuth (distances ranging from 350 to 400 km) , the seismograms recorded in Compton (the central part of the basin), Long Beach (the southern edge of the basin), and downtown Los Angeles are remarkably different, even for a common explosion. Following the onset of L(g) waves, the Long Beach sites have recorded surface waves for more than 100 sec. From one explosion, the sites within downtown L os Angeles have recorded seismograms with strong 3-sec surface waves. These waves are not observed on the seismograms recorded in the neighb oring hard-rock site California Institute of Technology (CIT) station. Thus, they must have been generated by local wave guides. Numerically , we modeled these 3-sec waves by convolving the CIT seismogram with t he response of a sedimentary strata dipping gently (about 6-degrees) f rom CIT toward downtown. We also examined the irregular basin effect b y analyzing the variation of cumulative temporal energy across the bas in relative to the energy recorded at CIT from the same explosion. Var iation up to a factor of 30 was observed. To model the energy variatio n that is caused by extended surface waves in the Long Beach area, we used numerically simulated site transfer functions (STF) from a NNE-SS W oriented two-dimensional basin structure extending from Montebello t o Palos Verdes that included low-velocity sedimentary material in the uppermost layers. These STFs were convolved with the CIT seismogram re corded from the MAST explosion. To simulate elongated duration of surf ace waves, we introduced in the upper sedimentary structure some disco ntinuous microbasin structures of varying size, each microbasin delayi ng the seismic waves propagating through them. Consequently, the surfa ce-reflected phases through these structures are delayed and reflected into the upper medium by the underlying interfaces. This mechanism he lps delayed energy to appear at a later time and result in a longer ti me duration at sites located at southern edge of the basin.