Structural geological data of the Yunodake Fault in southeastern Fukushima Prefecture, NE Japan

Table S1. Fault-slip data from fault tips in the Yunodake Fault zone and misfit angles under stress states estimated by multiple inverse method analysis. Sense of shear was estimated from composite planar fabrics and kinematic indicators on slickensides. *: Misfit angle less than 30°. Table S2. Fault-slip data from the Nakano-kita outcrop of the Yunodake Fault and misfit angles under stress states estimated by multiple inverse method analysis. Sense of shear was estimated from composite planar fabrics and kinematic indicators on slickensides. *: Misfit angle less than 30°. Table S3. Fault-slip data from the Kanzawa outcrop of the Yunodake Fault and misfit angles under stress states estimated by multiple inverse method analysis. Sense of shear was estimated from composite planar fabrics and kinematic indicators on slickensides. *: Misfit angle less than 30°. Table S4. Fault-slip data from the Iritonodam-kita outcrop of the Yunodake Fault and misfit angles under stress states estimated by multiple inverse method analysis. Sense of shear was estimated from composite planar fabrics and kinematic indicators on slickensides. *: Misfit angle less than 30°.