Fault zone amplified waves as a possible seismic hazard along the Calaveras fault in central California

Geophysical Research Letters

Volumn 28, Issue 13, 2001, Pages 2533-2536

  Spudich, P ^a   Olsen, K B ^b  

^a U S GEOLOGICAL SURVEY   (United States)

^b UNIVERSITY OF CALIFORNIA   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

COMPUTER SIMULATION; EARTHQUAKES; VELOCITY; WAVE EFFECTS; HAZARDS; SEISMIC RESPONSE; SEISMOLOGY;

LOW VELOCITY ZONE (LVZ);

SEISMOLOGY; EARTHQUAKES;

AMPLIFICATION; EARTHQUAKE; FAULT ZONE; NATURAL HAZARD; SEISMIC HAZARD; SEISMIC WAVE;

UNITED STATES;

CALIFORNIA; FAULT ZONE; GROUND MOTIONS; LOMA PRIETA EARTHQUAKES; LOW VELOCITY ZONES; SEISMIC HAZARDS; SURFACE TRACES; VELOCITY PULSE;

EID: 0035392469     PISSN: 00948276     EISSN: None     Source Type: Journal    
DOI: 10.1029/2000GL011902     Document Type: Article

References (13)

1. Linearized inversion for fault rupture behavior: Application to the 1984 Morgan Hill, California, earthquake
2. Internal structure and weakening mechanisms of the San Andreas fault
3. Amplification of ground motion and waveform complexity in fault zones: Examples from the San Andreas and Calaveras fault zones
4. The attenuation of seismic shear waves in quaternary alluvium in Santa Clara Valley, California
5. Rupture history of the 1984 Morgan Hill, California, earthquake from the inversion of strong ground motion records
6. Seismic guided waves trapped in the fault zone of the Landers, California, earthquake of 1992
7. San Jacinto fault zone guided waves: A discrimination for recently active fault strands near Anza, California
8. The near-source ground motion of the 6 August 1979 Coyote Lake, California
9. Vertical seismic profiling of Oroville microearthquakes: Velocity spectra and particle motion as a function of depth
10. Viscoelastic finite-difference modeling