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Earthquake Research Institute, University of Tokyo | 論文
- Time variation of the electromagnetic transfer function of the earth estimated by using wavelet transform
- Development of instruments for seafloor geodesy
- ESTIMATION OF MAXIMUM DISPLACEMENT RESPONSE OF REINFORCED CONCRETE STRUCTURES BASED ON ENERGY INPUT RATE SPECTRUM
- Diffusion of crustal deformation from disturbances arising at plate boundaries : a case of the detachment beneath the Izu Peninsula, central Honshu, Japan
- Tidal influence on the 2000 Miyake jima eruption and its implications for hydrothermal activity and volcanism
- The seismogenic zone of subduction thrust faults
- Lithium, strontium, and neodymium isotopic compositions of oceanic island basalts in the Polynesian region : constraints on a Polynesian HIMU origin
- Investigation of the Onikobe geyser, NE Japan, by observing the ground tilt and flow parameters
- P57 Changes in stress accompanying the 2004 eruption of Mt. Asama, Japan as measured by seismic anisotropy and GPS
- Constraints on HIMU and EM by Sr and Nd isotopes re-examined
- Criticality and Scaling Relations in a Sheared Granular Material(General)
- Criticality and Scaling Relations in a Sheared Granular Material
- Construction of I-Xe and ^Ar-^Ar Dating System Using a Modified VG3600 Mass Spectrometer and the First I-Xe Data Obtained in Japan
- Crack-filling clays and weathered cracks in the DPRI 1800m core near the Nojima Fault, Japan : Evidence for deep surface-water circulation near an active fault
- Evidence of primitive melt heterogeneities preserved in plagioclase-hosted melt inclusions of South Atlantic MORB
- EVALUATION OF THE DAMAGE TO WOODEN HOUSES CAUSED BY THE 1978 OFF-MIYAGI PREFECTURE EARTHQUAKE
- Estimation of the crustal structure and the bedrock topography by the gravitational method around Syowa Station, East Antarctica
- 3-A12 霧島火山群でのGPSによる地殻変動観測(桜島・霧島火山の活動2,口頭発表)
- K-Ar Dating of Volcanic Rocks Dredged from the Yamato Seamount Chain in the Japan Sea
- A Composite Diapir Model for Extensive Basaltic Volcanism : Magmas from Subducted Oceanic Crust Entrained within Mantle Plumes
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