Three-dimensional seismic velocity structure beneath Aso Volcano, Kyushu, Japan

Tomographic results for P- and S-wave velocity structure beneath the active Aso Volcano, Kyushu, Japan, using 800 well-recorded earthquakes and ten sh ots recorded by an eight-station seismic network, are presented. A 68% vari ance reduction was achieved upon simultaneous inversion for hypocenter and velocity structure. Well-resolved velocity anomalies associated with the ac tive crater reveal heterogeneity up to 26% slower and 18% faster in P veloc ity, and up to 31% slower and 22% faster in S velocity, than the one-dimens ional model. The largest anomaly is seen over the upper I I kin in the cent ral and northern parts beneath the central cones. Two low-velocity regions are imaged. The first region, a 10x15-km region encompassing the upper 3 km centered near the caldera wall at Tateno Valley, is characterized by P vel ocities up to 19% slower (20% for S). The second low-velocity region is ass ociated with the central cones and active magma conduit system at 6 km dept h. Velocities as low as 4.3 km/s (up to 26%) in P and 2 km/s (31% slower) i n S characterize the 7-km-wide volume. The magma chamber is roughly spheric al in shape, centered at 6 km depth, flattens at 10 kin depth, and is locat ed between Mt. Kishima, Mt. Eboshi, and Mt. Naka, the present focus of magm atism. A sharp velocity contrast at the depth of 3 kin, with high velocitie s to the southwest and lower velocities to the northeast, characterizes dif ferent abutting structures associated with the Oita-Kumamoto Tectonic Line.