Seismic velocity and attenuation structures in the top 400 km of the Earth's inner core along equatorial paths

@inproceedings{Yu2006SeismicVA,
  title={Seismic velocity and attenuation structures in the top 400 km of the Earth's inner core along equatorial paths},
  author={Wen-che Yu and Jennnifer Webb},
  year={2006}
}
[1] We study seismic velocity and attenuation structures in the top 400 km of the Earth's inner core based on modeling of differential traveltimes, amplitude ratios, and waveforms of the PKiKP-PKIKP phases observed at the epicentral distance range of 120°–141° and the PKPbc-PKIKP phases observed at the distance range of 146°–160° along equatorial paths. Our data are selected from the seismograms recorded in the Global Seismographic Network from 1990 to 2001 and many regional seismic networks… CONTINUE READING

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References

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