Source study of the 1906 San Francisco earthquake

@article{Wald1993SourceSO,
  title={Source study of the 1906 San Francisco earthquake},
  author={David J. Wald and Hiroo Kanamori and Donald V. Helmberger and Thomas H. Heaton},
  journal={Bulletin of the Seismological Society of America},
  year={1993}
}
All quality teleseismic recordings of the great 1906 San Francisco earthquake archived in the 1908 Carnegie Report by the State Earthquake Investigation Commission were scanned and digitized. First order results were obtained by comparing complexity and amplitudes of teleseismic waveforms from the 1906 earthquake with well calibrated, similarly located, more recent earthquakes (1979 Coyote Lake, 1984 Morgan Hill, and 1989 Loma Prieta earthquakes) at nearly co-located modern stations. Peak… 
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References

SHOWING 1-10 OF 26 REFERENCES
The location and source parameters of the Lompoc, California, earthquake of 4 November 1927
In this paper, we address the relocation, magnitudes, and the style of faulting of the Lompoc earthquake from a sparse assortment of teleseismic and regional seismograms. The highest quality
Waveform modeling of the November 1987 Superstition Hills earthquakes
Long-period body-wave data recorded at teleseismic distances and strong-motion data at Pasadena for the Superstition Hills earthquakes of 24 November 1987 are modeled to obtain the source parameters.
Strain accumulation and release mechanism of the 1906 San Francisco Earthquake
Reexamination of geodetic data has shown that significant crustal deformation both preceded and followed the great 1906 earthquake (M = 8.3). In the ∼50 years prior to 1906, tensor shear strain rates
The focus of the 1906 California earthquake
The location of the 1906 California earthquake is reexamined using both the P and S recordings at teleseismic distances and the local observations. Analysis of the observed travel times using modern
Rupture of the 4 February 1976 Guatemalan earthquake
Abstract An expanded body-wave data set for the 4 February 1976 Guatemalan earthquake is analyzed by iterative, multiple-station inversion to provide enhanced resolution of the rupture process of
Strong-motion recordings of the California earthquake of April 18, 1906
Recordings from a low magnification ( V = 4), intermediate period ( T ≈ 5 sec) seismograph at Mt. Hamilton, within 35 km of the San Andreas fault, show about 8 sec of P -wave energy and the first
Source mechanism of the 1906 San Francisco earthquake
The near-source ground motion of the 6 August 1979 Coyote Lake, California, earthquake
A finite fault striking N24°W and extending to a depth of 10 km is proposed to explain the strong ground motion data for the 6 August 1979 Coyote Lake, California, earthquake (M_L = 5.9). Our source
Strain accumulation on the northern San Andreas Fault Zone since 1906
Post-1906 geodetic surveys in the region of the great San Francisco earthquake have provided some details on the pattern and mechanism of the strain accumulation now occurring between 37° and 38°N on
Rupture model of the 1989 Loma Prieta earthquake from the inversion of strong-motion and broadband teleseismic data
We have used 24 broadband teleseismic and 48 components of local strong-motion velocity records of the 1989 Loma Prieta earthquake in a formal inversion to determine the temporal and spatial
...
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