Published May 20, 2005
| Supplemental Material
Journal Article
Open
The Great Sumatra-Andaman Earthquake of 26 December 2004
Abstract
The two largest earthquakes of the past 40 years ruptured a 1600-kilometer-long portion of the fault boundary between the Indo-Australian and southeastern Eurasian plates on 26 December 2004 [seismic moment magnitude (M_w) = 9.1 to 9.3] and 28 March 2005 (M_w = 8.6). The first event generated a tsunami that caused more than 283,000 deaths. Fault slip of up to 15 meters occurred near Banda Aceh, Sumatra, but to the north, along the Nicobar and Andaman Islands, rapid slip was much smaller. Tsunami and geodetic observations indicate that additional slow slip occurred in the north over a time scale of 50 minutes or longer.
Additional Information
© 2005 American Association for the Advancement of Science. Received 14 March 2005; accepted 25 April 2005. This work was supported in part by the U.S. National Science Foundation under grants EAR-0125595, EAR-0337495, and EAR-0207608. Seismic waveform data from the Global Seismographic Network (funded by NSF under Cooperative Agreement EAR-0004370 and USGS) were obtained from the Incorporated Research Institutions for Seismology (IRIS) Data Management System. Jason data were provided by Lee-Lueng Fu of the Jet Propulsion Laboratory in Pasadena, CA.Attached Files
Supplemental Material - 1112250s1.mov
Supplemental Material - 1112250s2.mov
Supplemental Material - Lay_SOM.pdf
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Additional details
- Eprint ID
- 20879
- Resolver ID
- CaltechAUTHORS:20101118-091748150
- EAR-0125595
- NSF
- EAR-0337495
- NSF
- EAR-0207608
- NSF
- Created
-
2010-11-18Created from EPrint's datestamp field
- Updated
-
2023-04-19Created from EPrint's last_modified field
- Caltech groups
- Caltech Tectonics Observatory, Division of Geological and Planetary Sciences
- Other Numbering System Name
- Caltech Tectonics Observatory
- Other Numbering System Identifier
- 16