Khan, Prosanta K...[ et al.]2018-06-152018-06-152012Geoscience Frontiers, 2012, V.3(No.4), P.241-267https://doi.org/10.1016/j.gsf.2011.11.012http://hdl.handle.net/123456789/1244enFlexing zoneNon-coaxial deformationShear crackNeutral surfaceRheologyCompressive stressSCIETesting the intraplate origin of mega-earthquakes at subduction marginsArticle