Long period microtremors, microseisms and earthquake damage: Northridge, CA, earthquake of 17 January 1994 |
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| Authors: | M D Trifunac M I Todorovska |
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| Institution: | Civil Engineering Department, University of Southern California, Los Angeles, CA 90089-2531, USA |
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| Abstract: | Three studies of site amplification factors, based on the recorded aftershocks, and one study based on strong motion data, are compared one with another and with the observed distribution of damage from the Northridge, CA, earthquake of 17 January 1994 (ML=6.4). In the epicentral area, when the peak ground velocities are larger than vm≈15 cm/s, nonlinear response of soil begins to distort the amplification factors determined from small amplitude (linear) wave motion. Moving into the area of near-field and strong ground motion (vm>30 cm/s), the site response becomes progressively more affected by the nonlinear soil response. Based on the published results, it is concluded that site amplification factors determined from small amplitude waves (aftershocks, small earthquakes, coda waves) and their transfer-function representation may be useful for small and distant earthquake motions, where soils and structures respond to earthquake waves in a linear manner. However in San Fernando Valley, during the Northridge earthquake, the observed distribution of damage did not correlate with site amplification determined from spectra of recorded weak motions. Mapping geographical distribution of site amplification using other than very strong motion data, therefore appears to be of little use for seismic hazard analyses. |
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| Keywords: | Northridge earthquake Aftershocks Site amplification Site response Microzonation Seismic hazard Seismic hazard mapping |
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