We present differential bathymetry and sediment core data from the Japan Trench, sampled after the 2011 Tohoku-Oki earthquake to document that prominent bathymetric and structural changes along the trench axis relate to a large (~27.7 km 2 ) slump in the trench.Transient geochemical signals in the slump deposit and analyzing diffusive re-equilibration of disturbed
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Strasser et al. (2013) studied this question.
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