All Supporting Information may be found in the online version of this article.
3-D active source tomography around Simeulue Island offshore Sumatra: Thick crustal zone responsible for earthquake segment boundary
Article first published online: 15 JAN 2013
©2013 American Geophysical Union. All Rights Reserved.
Geophysical Research Letters
Volume 40, Issue 1, pages 48–53, 16 January 2013
How to Cite
2013), 3-D active source tomography around Simeulue Island offshore Sumatra: Thick crustal zone responsible for earthquake segment boundary, Geophys. Res. Lett., 40, 48–53, doi:10.1029/2012GL054148., , , , , , , , , , and (
- Issue published online: 29 JAN 2013
- Article first published online: 15 JAN 2013
- Manuscript Accepted: 29 NOV 2012
- Manuscript Revised: 27 NOV 2012
- Manuscript Received: 8 OCT 2012
- Natural Environment Research Council. Grant Number: NE/D004381/1
Supporting information may be found in the online version of this article.
|2012gl054148fs01.tif||TIFF image||5489K||Figure S1. Depth-migrated MCS profile SUMAE05 with the top of the oceanic crust (TOC) picks (red dots) superimposed. Location of the profile is indicated in the figure ¡°2012gl054148-fs02.tif¡±.|
|2012gl054148fs02.tif||TIFF image||622K||Figure S2. Locations of the acquired MCS data profiles (purple lines) in our survey (SO198-2) and the positions of the TOC picks from these profiles (black dots) and from the MCS profiles (red dots) published by Franke et al. .|
|2012gl054148fs03.tif||TIFF image||1153K||Figure S3. OBS A09 (a) in-line and (b) off-line profile sections with seismic phases labeled. (inset) Locations of OBS A09 and the profile sections. Pap: P-wave refracted in the accretionary prism; Pg': P-wave refracted in the backstop block; Pn: P-wave refracted in the oceanic mantle; PcP: P-wave reflected at the top of the oceanic crust; PmP: P-wave reflected at the oceanic Moho surface.|
|2012gl054148fs04.tif||TIFF image||1042K||Figure S4. OBS A30 (a) in-line and (b) off-line profile sections with seismic phases labeled. (inset) Locations of OBS A30 and the profile sections. Ps': P-wave refracted in the shallow sediment layer; Pg': P-wave refracted in the backstop block.|
|2012gl054148fs05.tif||TIFF image||2226K||Figure S5. Velocity cross-sections extracted from the 3-D initial velocity model used for the final travel-time inversion. (a) vertical cross-sections perpendicular to the trench; (b) vertical cross-sections parallel to the trench; (c) Location of these cross-sections.|
|2012gl054148fs06.tif||TIFF image||604K||Figure S6. The distribution of the residuals between the travel-times calculated from the initial model and the picked travel-times.|
|2012gl054148fs07.tif||TIFF image||561K||Figure S7. The distribution of the final residuals of the travel-times used in the inversion. Blue lines indicate the uncertainty level assigned to the travel-times according to their source-receiver offset.|
|2012gl054148fs08.tif||TIFF image||559K||Figure S8. The root-mean-squares residual of the travel-time inversion over successive iterations. Convergence is reached after 22 iterations.|
|2012gl054148fs09.tif||TIFF image||641K||Figure S9. 3-D ray-paths traced through the final velocity model inverted from the first-arrival travel-time tomography (every 50th ray-path plotted).|
|2012gl054148fs10.tif||TIFF image||1113K||Figure S10. Checkerboard tests. Recovered velocity anomaly patterns at different depth for anomaly size 40, 30, 20, and 10 km (from left to right), respectively.|
|2012gl054148fs11.tif||TIFF image||883K||Figure S11. Checkerboard tests. Recovered velocity anomaly patterns in vertical cross-sections perpendicular to the trench (a) and parallel to the trench (b) for anomaly size 40 km × 5 km. (c) Locations of these cross-sections.|
|2012gl054148fs12.tif||TIFF image||2649K||Figure S12. The velocity variations relative to the averaged along-strike velocities at fixed depths from the top of the oceanic crust, projected on a horizontal plane. The purple line, approximating the zero velocity variations, outline the anomalous velocity zone. Note the consistent low velocity anomaly in the subducting plate as it approaches the 2004–2005 rupture segment boundary. Red star: the 2004 Mw 9.2 earthquake; Green star: the 2005 Mw 8.7 earthquake; Yellow stars and Black dots: seismicity during 1964–2007 (from EHB catalogue). Depth bel. inf.= depth below the top of the oceanic crust.|
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.