スポンサーリンク
東京帝国大学地震研究所,Earthquake Research Institute, Tokyo Imperial University,Earthquake Research Institute. | 論文
- 58.Determination of Elastic Constants of Soils by means of Vibration Methods. : Part I. Young's Modulus.
- 7.Determination of Elastic Constants of Soils by means of Vibration Methods. : Part 2. Modulus of Rigidity and Poisson's Ratio.
- 31.Damping in Seismic Vibrations of a Surface Layer due to an Obliquely Incident Disturbance.
- 46.Energy Dissipation in Seismic Vibrations of an Eight-storied Structure.
- 1.Resonance Phenomena and Dissipation Waves in the Stationary Vibrations of a Semi-infinite Body.
- 11.Energy Dissipation in Seismic Vibrations of Actual Buildings of Unlike Structure.
- 32.Dissipation Waves Accompanying Forced Seiches in a Bay.
- 34.Energy Dissipation in Seismic Vibrations of Actual Buildings Predicted by means of an Improved Theory.
- 22.The Same Stationary Vibration of an Origin Accompanying Different Types of Disturbances Therefrom.
- 18.On a Problem Concerning the Internal Structure of the Earth as Discussed from the Time-distance Curve of the Formosa Earthquake of April 20, 1935.
- 14.Statistic Investigations of Earthquake Frequencies.
- 52.Notes on the Origins of Earthquakes.
- 50.Experimental Studies on the Deformation of Sand Masses due to Vertical Loads. I.
- 51.Tunami associated with the Sanriku Earthquake thai occurred on November 3, 1936.
- 27.Tilt Observations during the Recent Activities of Volcano Asama.
- 6.Torsion Balance Surveys on Volcano Asama. (Part 1.)
- 41.Geology and Petrography of lo-sima (Sulphur Island), Volcano Islands Group.
- 20.On the Volcanism of the Huzi Volcanic Zone, with Special Reference to the Geology and Petrology of Idu and the Southern Islands.
- 60.The Arrangement of Layers in the Earth's Oust as deduced from Seismometrical Observations at Hongo, Tokyo (first paper)
- 30.Theoretical and Experimental Study of Initial Motion of Seismographs and the Quantitative Study of First Impulsion of Earthquake. : Part II.-An Experimental. Study of the Initial Motion of Seismographs caused by Motions of Short Duration.