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|Title:||Postseismic relaxation in Kashmir and lateral variations in crustal architecture and materials||Authors:||Bendick, R.
Khan, S. F.
Khan, M. A.
|Keywords:||DRNTU::Science::Geology::Volcanoes and earthquakes||Issue Date:||2015||Source:||Bendick, R., Khan, S. F., Bürgmann, R., Jouanne, F., Banerjee, P., Khan, M. A., et al. (2015). Postseismic relaxation in Kashmir and lateral variations in crustal architecture and materials. Geophysical research letters, 42(11), 4376-4383.||Series/Report no.:||Geophysical research letters||Abstract:||Thirty horizontal displacement time series from GPS sites in the area around the 2005 Kashmir earthquake show lateral spatial variations in displacement magnitude and relaxation time for the postseismic interval from 2005 to 2012. The observed spatial pattern of surface displacements can only be reproduced by finite element models of postseismic deformation in elastic over viscoelastic crust that include lateral differences in both the thickness of the elastic layer and the viscosity of the viscoelastic layer. Solutions reproducing the sign of horizontal displacements everywhere in the epicentral region also require afterslip on the portion of the fault dislocation in the viscoelastic layer but not in the elastic lid. Although there are substantial tradeoffs among contributions to postseismic displacements of the surface, the observations preclude both crustal homogeneity and shallow afterslip. In the best family of solutions, the thickness of the elastic upper crust differs by a factor of 5 and the viscosity of the middle and lower crust by an order of magnitude between domains north and south of a suture zone containing the Main Boundary Thrust and Main Mantle Thrust.||URI:||https://hdl.handle.net/10356/79381
|ISSN:||0094-8276||DOI:||10.1002/2015GL064670||Research Centres:||Earth Observatory of Singapore||Rights:||© 2015 American Geophysical Union. This paper was published in Geophysical Research Letters and is made available as an electronic reprint (preprint) with permission of American Geophysical Union. The published version is available at: [http://dx.doi.org/10.1002/2015GL064670]. 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|
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