Measuring finite-frequency body-wave amplitudes and traveltimes
We have developed a method to measure finite-frequency amplitude and traveltime anomalies of teleseismic P waves. We use a matched filtering approach that models the first 25 s of a seismogram after the P arrival, which includes the depth phases pP and sP. Given a set of broad-band seismograms from...
Váldodahkkit: | , |
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Materiálatiipa: | Journal article |
Giella: | English |
Almmustuhtton: |
2006
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