1989 Volume 1989 Issue 14B Pages 11-24
We examined the characteristics of the ground structure of the Karoeoka, Kyoto, Osaka basins and the Kumamoto Plain based or the boring database system of the areas with respect to: distribution of facies at the same elevations and depths; three dimensional projection of geological columns; distribution of the upper surface depth of pyroclastic flow deposits (ASO-4) ; calculation of appearance percentage of clay, sand and gravel at the same elevations and at 0.5m-intervals; Markov matrix which quantifies the transitions of facies: and distribution of N values in clay or sand at the same depths.