New insights on the offshore extension of the Great Sumatran fault, NW Sumatra, from marine geophysical studies
Article first published online: 29 NOV 2012
Published in 2012 by the American Geophysical Union
Geochemistry, Geophysics, Geosystems
Volume 13, Issue 11, November 2012
How to Cite
2012), New insights on the offshore extension of the Great Sumatran fault, NW Sumatra, from marine geophysical studies, Geochem. Geophys. Geosyst., 13, Q0AF06, doi:10.1029/2012GC004122., , , and (
- Issue published online: 29 NOV 2012
- Article first published online: 29 NOV 2012
- Manuscript Accepted: 17 OCT 2012
- Manuscript Revised: 20 SEP 2012
- Manuscript Received: 24 FEB 2012
Auxiliary material for this article contains a text file and seven high resolution figures to identify the faults on bathymetry and single channel profiles and to describe the methodology applied during the processing of the wide angle seismic reflection datasets.
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Additional file information is provided in the readme.txt.
|ggge2324-sup-0001-readme.txt||plain text document||3K||readme.txt|
|ggge2324-sup-0002-txts01.txt||plain text document||48K||Text S1. The methodologies for downward continuation, travel time tomography and pre-stack depth migration.|
|ggge2324-sup-0003-fs01.png||PNG image||1961K||Figure S1. Uninterpreted bathymetry.|
|ggge2324-sup-0004-fs01.pdf||PDF document||1961K||Figure S2. Downward continuation technique.|
|ggge2324-sup-0005-fs03.tif||TIFF image||3137K||Figure S3. Two downward continued shot gathers at two different locations, their starting and final travel time misfits and corresponding ray paths in final velocity models.|
|ggge2324-sup-0006-fs04.tif||TIFF image||704K||Figure S4. The data misfits as a function of model roughness showing L-shaped curve.|
|ggge2324-sup-0007-fs05.tif||TIFF image||183K||Figure S5. Histogram of the data errors for all shots and receiver.|
|ggge2324-sup-0008-fs06.pdf||PDF document||1467K||Figure S6. Uninterpreted single channel profiles.|
|ggge2324-sup-0009-fs07.tif||TIFF image||2383K||Figure S7. The time section of a CDP gather of the 5.5 km streamer located in the Breueh Basin and the common image point gather marked in Figure 7b.|
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