Along-strike variations in the Nankai shallow décollement properties and their implications for tsunami earthquake generation
Author:
Affiliation:
1. Atmosphere and Ocean Research Institute; University of Tokyo; Kashiwa Japan
2. Department of Geology and Mineralogy; Kyoto University; Kyoto Japan
3. Institute for Geophysics; University of Texas; Austin Texas USA
Funder
MEXT
Publisher
American Geophysical Union (AGU)
Subject
General Earth and Planetary Sciences,Geophysics
Link
http://onlinelibrary.wiley.com/wol1/doi/10.1002/2014GL061096/fullpdf
Reference40 articles.
1. Source mechanisms and tectonic significance of historical earthquakes along the Nankai trough, Japan;Ando;Tectonophysics,1975
2. Broad, weak regions of the Nankai megathrust and implications for shallow coseismic slip;Bangs;Earth Planet. Sci. Lett.,2009
3. Tsunami earthquakes possibly widespread manifestations of frictional conditional stability;Bilek;Geophys. Res. Lett.,2002
4. Fracture porosity in the décollement zone of Nankai accretionary wedge using Logging While Drilling resistivity data;Bourlange;Earth Planet. Sci. Lett.,2003
5. Evidence for a weak and overpressured décollement beneath sediment-dominated accretionary prisms;Byrne;J. Geophys. Res.,1990
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