Crustal and uppermost mantle structure of southern Norway: results from surface wave analysis of ambient seismic noise and earthquake data
Article first published online: 19 OCT 2012
© 2012 The Authors Geophysical Journal International © 2012 RAS
Geophysical Journal International
Volume 191, Issue 3, pages 1441–1456, December 2012
How to Cite
Köhler, A., Weidle, C. and Maupin, V. (2012), Crustal and uppermost mantle structure of southern Norway: results from surface wave analysis of ambient seismic noise and earthquake data. Geophysical Journal International, 191: 1441–1456. doi: 10.1111/j.1365-246X.2012.05698.x
- Issue published online: 12 NOV 2012
- Article first published online: 19 OCT 2012
- Accepted 2012 September 24. Received 2012 September 12; in original form 2012 March 2
Figure S1. Rayleigh wave phase velocity dispersion curves for four station pairs obtained by time frequency analysis. Locations of receivers and corresponding noise cross-correlation functions (20-month stacks, scale is in seconds) are shown. Thick black line indicates dispersion curve averaged over all 3-month stacks. Thin lines show standard deviation. Colored lines represent dispersion curve obtained from cross-correlation stacks over entire record (red), over summer months (green, June to August), and over winter months (blue, November to January), respectively.
Figure S2. Same as Fig. S1 for Love waves.
Figure S3. Rayleigh and Love wave phase velocity maps at selected periods obtained by phase interpolation of earthquake observations using MAGNUS data only. White dashed lines indicate resolution limits: relative sampling contour of three (number of velocity estimates by number of nodes).
|GJI_5698_sm_FiguresS1-S3.zip||237K||Supporting info item|
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