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• W1979730228 abstract "Deformation bands in argillaceous sediments at the toe of the Nankai accretionary prism are roughly planar, ∼1–10 mm thick, bedding-oblique zones. The bands are typically developed as two oppositely dipping sets. A band of one set can be displaced by the slickenlined surface of the oppositely dipping band, showing a reverse slip with respect to a horizontal plane. Deformation bands commonly consist of thinner subbands that are oblique or parallel to the boundaries of the deformation bands. The subbands also display a reverse slip with respect to a horizontal plane, and particles within subbands are oriented perpendicular to the maximum principal stress (σ1), regardless of the dips of the subbands. Physical property analysis using an X-ray computed tomography scanner demonstrates that porosity reduction in the deformation bands relative to the surrounding undeformed material ranges from 1 to 6%. The deformation bands are compactive shear bands formed under subhorizontal σ1 associated with northwest-directed plate convergence, and subbands arise from a combination of reverse sense of shear and flattening perpendicular to σ1, with their geometries producing the S–C aspect observed in sheared clayey sediments or ductile metamorphic shear zones." @default.
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• W1979730228 date "2004-02-01" @default.
• W1979730228 modified "2023-09-26" @default.
• W1979730228 title "Origin of deformation bands in argillaceous sediments at the toe of the Nankai accretionary prism, southwest Japan" @default.
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• W1979730228 doi "https://doi.org/10.1016/j.jsg.2003.06.001" @default.
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