Large amplitude variations recorded by an on-fault seismological station during the L'Aquila earthquakes: Evidence for a complex fault-induced site effect
Version of Record online: 23 DEC 2010
Copyright 2010 by the American Geophysical Union.
Geophysical Research Letters
Volume 37, Issue 24, December 2010
How to Cite
2010), Large amplitude variations recorded by an on-fault seismological station during the L'Aquila earthquakes: Evidence for a complex fault-induced site effect, Geophys. Res. Lett., 37, L24305, doi:10.1029/2010GL045697., , and (
- Issue online: 23 DEC 2010
- Version of Record online: 23 DEC 2010
- Manuscript Accepted: 15 NOV 2010
- Manuscript Revised: 4 NOV 2010
- Manuscript Received: 30 SEP 2010
Auxiliary material for this article contains figure of relevant features dealing with properties of trapped waves recorded at FAGN.
Auxiliary material files may require downloading to a local drive depending on platform, browser, configuration, and size. To open auxiliary materials in a browser, click on the label. To download, Right-click and select “Save Target As…” (PC) or CTRL-click and select “Download Link to Disk” (Mac).
Additional file information is provided in the readme.txt.
|grl27654-sup-0001-readme.txt||plain text document||2K||Readme.txt|
|grl27654-sup-0002-fs01.pdf||PDF document||15063K||Figure S1. The unconsolidated soft upper layer indicated by boreholes does not play a role on the observed amplification at FAGN.|
|grl27654-sup-0003-fs02.pdf||PDF document||886K||Figure S2. A second large-amplitude phase arrives about 1 sec after the direct S waves for source distances of 11 to 13 km.|
|grl27654-sup-0004-fs03.pdf||PDF document||807K||Figure S3. As in Figure S2 but the time delay increases up to 2 sec for distances of 21 to 25 km. In the paper, we use this time delay to constrain geometry and velocity of the fault zone model.|
|grl27654-sup-0005-fs04.pdf||PDF document||250K||Figure S4. Describes how the misfit between the theoretical and observed fault zone spectrum changes for different model parameters.|
Please note: Wiley Blackwell is not responsible for the content or functionality of any supporting information supplied by the authors. Any queries (other than missing content) should be directed to the corresponding author for the article.