Article ID Journal Published Year Pages File Type
4693027 Tectonophysics 2011 13 Pages PDF
Abstract
► Impact of collision in the Hidaka Collision Zone is evident as biaxial stress. ► At the shallower part of the subduction zone uniaxial compression is dominant. ► Past large earthquakes are located in the strong fault segments.
Keywords
Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Earth-Surface Processes
Preview
Spatial distribution of stress and frictional strength along the interplate boundary in northern Japan and its correlation to the locations of large earthquakes
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