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Plate-boundary deformation associated with the great Sumatra–Andaman earthquake

Subarya, Cecep and Chlieh, Mohamed and Prawirodirdjo, Linette and Avouac, Jean-Philippe and Bock, Yehuda and Sieh, Kerry and Meltzner, Aron J. and Natawidjaja, Danny H. and McCaffrey, Robert (2006) Plate-boundary deformation associated with the great Sumatra–Andaman earthquake. Nature, 440 (7080). pp. 46-51. ISSN 0028-0836. doi:10.1038/nature04522. https://resolver.caltech.edu/CaltechAUTHORS:20101117-111421546

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Abstract

The Sumatra–Andaman earthquake of 26 December 2004 is the first giant earthquake (moment magnitude M_w > 9.0) to have occurred since the advent of modern space-based geodesy and broadband seismology. It therefore provides an unprecedented opportunity to investigate the characteristics of one of these enormous and rare events. Here we report estimates of the ground displacement associated with this event, using near-field Global Positioning System (GPS) surveys in northwestern Sumatra combined with in situ and remote observations of the vertical motion of coral reefs. These data show that the earthquake was generated by rupture of the Sunda subduction megathrust over a distance of >1,500 kilometres and a width of <150 kilometres. Megathrust slip exceeded 20 metres offshore northern Sumatra, mostly at depths shallower than 30 kilometres. Comparison of the geodetically and seismically inferred slip distribution indicates that ~30 per cent additional fault slip accrued in the 1.5 months following the 500-second-long seismic rupture. Both seismic and aseismic slip before our re-occupation of GPS sites occurred on the shallow portion of the megathrust, where the large Aceh tsunami originated. Slip tapers off abruptly along strike beneath Simeulue Island at the southeastern edge of the rupture, where the earthquake nucleated and where an M_w = 7.2 earthquake occurred in late 2002. This edge also abuts the northern limit of slip in the 28 March 2005 M_w = 8.7 Nias–Simeulue earthquake.


Item Type:Article
Related URLs:
URLURL TypeDescription
http://dx.doi.org/10.1038/nature04522 DOIArticle
http://www.nature.com/nature/journal/v440/n7080/full/nature04522.htmlPublisherArticle
http://rdcu.be/clOJPublisherFree ReadCube access
ORCID:
AuthorORCID
Avouac, Jean-Philippe0000-0002-3060-8442
Sieh, Kerry0000-0002-7311-2447
Meltzner, Aron J.0000-0002-2955-0896
Additional Information:© 2006 Nature Publishing Group. Received 20 July; accepted 9 December 2005. We thank the team from BAKOSURTANAL who collected the GPS field data in Sumatra under difficult conditions (J. Efendi, A. Indrajit, M. Nyamadi, C. Bagandi, D. Sudharmono, A. Suryono, M. Achmad, U. Santoso, C. Yuniarsa, Endang, A. Pujobuntoro, H. Dradjat, B. Susilo and B. Parjanto). We are grateful to C. Vigny for comments and suggestions. This work has benefited from discussions with C. Ji. The Gordon and Betty Moore Foundation, the US National Science Foundation, the Southern California Earthquake Center, and BAKOSURTANAL supported this research. We thank R. W. Matindas and J. McRaney for their support. This is Caltech Tectonics Observatory contribution number 31.
Group:Caltech Tectonics Observatory, Caltech Tectonics Observatory. Sumatran Plate Boundary, Seismological Laboratory
Funders:
Funding AgencyGrant Number
Gordon and Betty Moore FoundationUNSPECIFIED
NSFUNSPECIFIED
Southern California Earthquake CenterUNSPECIFIED
BAKOSURTANALUNSPECIFIED
Other Numbering System:
Other Numbering System NameOther Numbering System ID
Caltech Tectonics Observatory31
Issue or Number:7080
DOI:10.1038/nature04522
Record Number:CaltechAUTHORS:20101117-111421546
Persistent URL:https://resolver.caltech.edu/CaltechAUTHORS:20101117-111421546
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:20858
Collection:CaltechAUTHORS
Deposited By: Tony Diaz
Deposited On:17 Nov 2010 19:26
Last Modified:09 Nov 2021 00:03

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