Research Project
Grant-in-Aid for Young Scientists (B)
Change in deformation styles and the related transition from smectite to illite within the aseismic-seismic transition zone (2-4 km below the seafloor) in a subduction zone were analyzed by studying an onland accretionary complex that was previously buried to a depth of just 2-4 km. Such strain hardening associated with the clay mineral transition and decrease in porosity is the primary mechanism of thickening of the decollement and/or melange zone, and represents a fundamental mechanical/chemical change in the properties of sediments immediately before entering the seismogenic zone.
All 2011 2010 2009 Other
All Journal Article (12 results) (of which Peer Reviewed: 11 results) Presentation (27 results)
Advances in Natural and Technological Hazards Research
Volume: (印刷中)
Tectonophysics 484
Pages: 156-167
120002949720
Tectonophysics 494
Pages: 75-84
月刊地球 号外61
Pages: 136-145
Tectonophysics
Volume: 484 Pages: 156-167
Boso accretionary complex. Central Japan. Island Arc 18
Pages: 496-512
Island Arc 18
Tectonophysics, TECTO07522. in press
Advances in Natural and Technological Hazards Research Series.(Springer) in press
Advances in Natural and Technological Hazards Research Series(Springer) in press