Field‐based description of near‐surface crustal deformation in a high‐strain shear zone: A case study in southern Kyushu, Japan

Abstract

AbstractThis study investigated geological evidence for near‐surface crustal deformation in a high‐strain shear zone that has been geodetically identified but which is not associated with obvious tectonic landforms. Fieldwork was conducted in the east–west‐trending southern Kyushu high‐strain shear zone (SKHZ), Japan, focusing mainly on occurrences of fracture zones, which are defined by a visible fracture density of >1 per 10 cm2 and are commonly associated with cataclasite, fault breccia, and gouge. The area in which east–west‐trending fracture zones are dominant is restricted to the east–west‐trending, ~2‐km‐wide aftershock area of the 1997 Northwestern Kagoshima Earthquakes. Analysis of slip data from minor faults using the multiple inverse method, irrespective of whether the faults are in fracture zones, reveals that the area where the calculated main stress field is consistent with the current stress field estimated from focal‐mechanism solutions of microearthquakes is restricted to the east–west‐trending aftershock area. This finding for the SKHZ contrasts with the case of the Niigata–Kobe Tectonic Zone, which is a major strain‐concentration zone with many exposed active faults in central Japan and for which the stress field estimated using fault‐slip data is considered to be uniform and coincides with the current stress field. The cumulative amount of displacement estimated from the areal density of fracture zones in the SKHZ study area is smaller than that estimated from geodetically measured strain rates. Investigations based on slip data from minor faults and fracture‐zone occurrence could help to identify concealed faults that are too small to generate tectonic landforms but which are sufficiently large to trigger major earthquakes.