Friction velocity dependence of clay-rich fault material along a megasplay fault in the Nankai subduction zone at intermediate to high velocities

• Published in: Geophysical research letters 2011-10, Vol.38 (19), p.n/a
• Main Authors: Tsutsumi, Akito, Fabbri, Olivier, Karpoff, Anne Marie, Ujiie, Kohtaro, Tsujimoto, Atsushi
• Format: Article
• Language: English
• Subjects: Clay; Continental dynamics; Deformation; Earth Sciences; Earth, ocean, space; Earthquakes; Environmental Sciences; Exact sciences and technology; fault gouge; Fault lines; Faults; Friction; frictional properties; Global Changes; Nankai Trough; Plate tectonics; Rheology; Sciences of the Universe; Seismic activity; Seismology; Slip velocity; splay fault; Subsidiaries; Surface layer; Tectonics; Texture
• ISSN: 0094-8276; 1944-8007
• DOI: 10.1029/2011GL049314

The frictional properties of clay‐rich fault material collected from a megasplay fault within the Nankai accretionary complex were examined in frictional experiments performed at a normal stress of 5 MPa under water‐saturated conditions for slip velocities from 0.0026 to 260 mm/s with >250 mm of displacement. Our results reveal that the fault material can show two stages of velocity weakening behavior: weakening at slow velocities (v < 2.6 mm/s), characterized by a small degree of friction velocity dependence (the absolute value of (a − b) is typically 26 mm/s). Such a process of fault weakening may provide important constraints on models of faulting along a megasplay fault. At slip velocities from 0.026 to 2.6 mm/s, there exist both velocity‐weakening and velocity‐strengthening fault materials. The frictional coefficient values, μ, for slow slip velocities (v = 0.26 mm/s) are relatively low (μ = 0.28–0.35) for velocity‐strengthening samples compared with velocity‐weakening samples (μ = 0.38–0.49). Microstructural analyses reveal that velocity‐strengthening samples show homogeneous deformation textures in which the entire gouge layer is deformed, whereas velocity‐weakening materials show evidence of shear localization in which deformation is concentrated along narrow subsidiary shears. Key Points Clay‐rich splay fault within the Nankai Trough exhibits velocity weakening The weakening could provide a condition to initiate unstable fault motion The velocity weakening may explain mechanism of the shallow VLF earthquakes