Upper Plate hysteresis controlling seismogenic rupture area, slow slip area in Subduction Zone; example from the Nankai Trough

Gaku Kimura, Department of Marine Resources and Environment, Tokyo University of Marine Science and Technology, Tokyo, Japan and Asuka Yamaguchi, Atmosphere and Ocean Research Institute, The University of Tokyo, Kashiwa, Japan
Back to: Slow Slip, Tectonic Tremor, and the Brittle-to-Ductile Transition Zone: What Mechanisms Control the Diversity of Slow and Fast Earthquakes? II