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|Title:||Piecemeal Rupture of the Mentawai Patch, Sumatra : The 2008 Mw 7.2 North Pagai Earthquake Sequence||Authors:||Salman, Rino
Hill, Emma Mary
Lindsey, Eric Ostrom
Mele Veedu, Deepa
Natawidjaja, Danny H.
|Issue Date:||2017||Source:||Salman, R., Hill, E. M., Feng, L., Lindsey, E. O., Mele Veedu, D., Barbot, S., et al. (2017). Piecemeal Rupture of the Mentawai Patch, Sumatra: The 2008 Mw 7.2 North Pagai Earthquake Sequence. Journal of Geophysical Research: Solid Earth, 122(11), 9404-9419.||Series/Report no.:||Journal of Geophysical Research: Solid Earth||Abstract:||The 25 February 2008 Mw 7.2 North Pagai earthquake partially ruptured the middle section of the Mentawai patch of the Sunda megathrust, offshore Sumatra. The patch has been forecast to generate a great earthquake in the next few decades. However, in the current cycle the patch has so far broken in a sequence of partial ruptures, one of which was the 2008 event, illustrating the potential of the patch to generate a spectrum of earthquake sizes. We estimate the coseismic slip distribution of the 2008 event by jointly inverting coseismic offsets from GPS and interferometric synthetic aperture radar. We then estimate afterslip with 5.6 years of cumulative GPS displacements. Our results suggest that the estimated afterslip partially overlaps the coseismic rupture. The overlap of coseismic rupture and afterslip can be explained conceptually by a simple rate‐and‐state model where the degree of overlapping is controlled by the dynamic weakening and the critical nucleation size in the velocity‐weakening area. Comparing our rate‐and‐state model results with our geodetic inversion results, we suggest that the part of the coseismic rupture that does not overlap with the afterslip may represent a velocity‐weakening region, while the overlapping part may represent a velocity‐strengthening region.||URI:||https://hdl.handle.net/10356/88585
|ISSN:||2169-9313||DOI:||10.1002/2017JB014341||Rights:||© 2017 American Geophysical Union (AGU). This paper was published in Journal of Geophysical Research : Solid Earth and is made available as an electronic reprint (preprint) with permission of American Geophysical Union (AGU). The published version is available at: [http://dx.doi.org/10.1002/2017JB014341]. One print or electronic copy may be made for personal use only. Systematic or multiple reproduction, distribution to multiple locations via electronic or other means, duplication of any material in this paper for a fee or for commercial purposes, or modification of the content of the paper is prohibited and is subject to penalties under law.||Fulltext Permission:||open||Fulltext Availability:||With Fulltext|
|Appears in Collections:||EOS Journal Articles|
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