不連續面が彈性波の傅播に及ぼす影響(其の7) : 表面層を有する彈性體内に於ける體自由波の生成及び傅播機構.雨彈性體が密着せる場合
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In the present paper are studied the vibratory motions of a surface layer and a subjacent semi-infinite elastic body when a dilatational wave is obliquely incident on the common boundary where the two solids adhere closely. In the first chapter, we studied the general properties of free waves propagated in the two solids, namely, in the surface layer and the subjacent solid, when a dilatational wave of harmonic wave-type of infinite extent is obliquely incident on the bottom surface of the surface layer. In the second chapter are explained analytically the general phenomena of wave motion in the two solids when a dilatational wave of shock wave-type is obliquely incident on the common boundary.
- 東京帝国大学地震研究所,Earthquake Research Institute, Tokyo Imperial University,地震研究所の論文
- 1935-09-30
東京帝国大学地震研究所,Earthquake Research Institute, Tokyo Imperial University,地震研究所 | 論文
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