Upper mantle P velocity structure beneath the Midwestern United States derived from triplicated waveforms
Version of Record online: 18 FEB 2012
Copyright 2012 by the American Geophysical Union
Geochemistry, Geophysics, Geosystems
Volume 13, Issue 2, February 2012
How to Cite
2012), Upper mantle P velocity structure beneath the Midwestern United States derived from triplicated waveforms, Geochem. Geophys. Geosyst., 13, Q0AK04, doi:10.1029/2011GC003818., , and (
- Issue online: 18 FEB 2012
- Version of Record online: 18 FEB 2012
- Manuscript Revised: 11 JAN 2012
- Manuscript Accepted: 11 JAN 2012
- Manuscript Received: 28 JUL 2011
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|ggge2088-sup-0001-readme.txt||plain text document||3K||readme.txt|
|ggge2088-sup-0002-fs01.pdf||PDF document||722K||Figure S1. Cut-and-Paste inversion of the Quebec earthquake determined by modeling regional broadband waveforms, which are arranged according to their azimuths.|
|ggge2088-sup-0003-fs02.pdf||PDF document||941K||Figure S2. CAP inversion of the focal mechanism for the Arkansas earthquake.|
|ggge2088-sup-0004-fs03.pdf||PDF document||798K||Figure S3. CAP inversion of the focal mechanism for the Oklahoma earthquake.|
|ggge2088-sup-0005-fs04.pdf||PDF document||604K||Figure S4. Comparison of stacked data with synthetics for the model CR.|
|ggge2088-sup-0006-fs05.pdf||PDF document||1148K||Figure S5. Sensitivity test of waveform fits for the perturbed models with different slopes above and below the low velocity zone.|
|ggge2088-sup-0007-fs06.pdf||PDF document||737K||Figure S6. Grid search for the structure of the 660 discontinuity.|
|ggge2088-sup-0008-fs07.pdf||PDF document||590K||Figure S7. Comparison of stacked data for southern stations and northern stations, which are separated by the line II in Figure 2.|
|ggge2088-sup-0009-fs08.pdf||PDF document||2091K||Figure S8. Record section of the Arkansas earthquake without and with travel-time corrections shown inFigure 12 with a reduce velocity of 8.3 km/s.|
|ggge2088-sup-0010-t01.txt||plain text document||1K||Tab-delimited Table 1.|
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