Low-velocity zone and topography as a source of site amplification effect on Tarzana hill, California
- 9 June 2008
- journal article
- Published by Elsevier
- Vol. 29 (2) , 324-332
- https://doi.org/10.1016/j.soildyn.2008.03.005
Abstract
No abstract availableKeywords
This publication has 10 references indexed in Scilit:
- Developing a Map of Geologically Defined Site-Condition Categories for CaliforniaBulletin of the Seismological Society of America, 2006
- Response of the Tarzana strong motion site during the 1994 Northridge earthquakePublished by Elsevier ,2002
- Shallow velocity structure and poisson's ratio at the Tarzana, California, strong-motion accelerometer siteBulletin of the Seismological Society of America, 1996
- The anomalous seismic response of the ground at the Tarzana hill site during the Northridge 1994 southern California earthquake: A resonant, sliding block?Bulletin of the Seismological Society of America, 1996
- Interpretation of significant ground-response and structure strong motions recorded during the 1994 Northridge earthquakeBulletin of the Seismological Society of America, 1996
- Directional topographic site response at Tarzana observed in aftershocks of the 1994 Northridge, California, earthquake: Implications for mainshock motionsBulletin of the Seismological Society of America, 1996
- Seismic response of a hill: The example of Tarzana, CaliforniaBulletin of the Seismological Society of America, 1996
- Directional Site Resonances Observed from the 1 October 1987 Whittier Narrows, California, Earthquake and the 4 October AftershockEarthquake Spectra, 1991
- The Whittier Narrows, California Earthquake of October 1, 1987—CSMIP Strong Motion DataEarthquake Spectra, 1988
- In-situ measurements of seismic velocity at 19 locations in the Los Angeles, California, regionOpen-File Report, 1981