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Complex tsunamigenic near-trench seafloor deformation during the 2011 Tohoku-Oki earthquake.


ABSTRACT: The near-trench coseismic rupture behaviour of the 2011 Tohoku-Oki earthquake remains poorly understood due to the scarcity of near-field observations. Differential bathymetry offers a unique approach to studying offshore coseismic seafloor deformation but has a limited horizontal resolution. Here we use differential bathymetry estimates with improved horizontal resolutions to investigate near-trench coseismic slip behaviours in the 2011 Tohoku-Oki earthquake. In the main rupture region, a velocity-strengthening behaviour in the shallow fault is observed. By contrast, the seafloor uplift decreases towards the trench, but the trend inverts near the backstop interface outcrop, revealing significant off-fault deformation features. Amongst various competing off-fault effects observed, we suggest that inelastic deformation plays a predominant role in near-trench tsunami excitation. Large trench-bleaching rupture is also observed immediately north of 39°, delimiting the northern extent of the main rupture region. Overall, striking spatial heterogeneity of the shallow rupture behaviour is revealed for the region.

SUBMITTER: Zhang K 

PROVIDER: S-EPMC10241807 | biostudies-literature | 2023 Jun

REPOSITORIES: biostudies-literature

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Complex tsunamigenic near-trench seafloor deformation during the 2011 Tohoku-Oki earthquake.

Zhang Kai K   Wang Yanru Y   Luo Yu Y   Zhao Dineng D   Wang Mingwei M   Yang Fanlin F   Wu Ziyin Z  

Nature communications 20230605 1


The near-trench coseismic rupture behaviour of the 2011 Tohoku-Oki earthquake remains poorly understood due to the scarcity of near-field observations. Differential bathymetry offers a unique approach to studying offshore coseismic seafloor deformation but has a limited horizontal resolution. Here we use differential bathymetry estimates with improved horizontal resolutions to investigate near-trench coseismic slip behaviours in the 2011 Tohoku-Oki earthquake. In the main rupture region, a veloc  ...[more]

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