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New F-K migrated multichannel reflection profiles establish the seismic stratigraphy between Sites 438/439 on the deep-sea terrace and Site 584 on the midslope terrace of the continental slope off Sanriku, northeastern Japan. Prominent downlappings of the basal strata are observed at places where the Cretaceous basement has been uplifted, and surface reflectors terminate or toplap at the same place. Uplift of the basement causes tensional stress and arching in the overlying Neogene strata along the outer margins of the midslope terrace and deep-sea terrace, forming both downlapping and toplapping. Graben within the subducted lithosphere may influence tectonic erosion along the base of the overlying prism.

Stratigraphy and Tectonic Interpretations of Multichannel Seismic Reflection Records across the Japan Trench off Sanriku, Northeastern Japan