University of Tsukuba, Department of Geosciences
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Affiliated Works
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- Behaviors of Zero Flux Planes and Soil Water Dynamics in a Pine Forest
- Development of Volcanic Plume Tracking Model 'PUFF' using Real-time Weather Data
- Mechanisms and Kinetics of the Post-Garnet Transformation in Pyrope
- Source of Metals and Genesis of Pb-Zn-Ag Deposits of Myanmar: Evidence from REE and Sulphur Isotopic Studies
- Tectonic implications for the occurrence of ocean floor, hotspot, and island arc materials within accretionary prisms: Examples from the Mesozoic-Cenozoic NW Pacific Rim
- The mode and nature of faulting and deformation and the emplacement history of the Mineoka ophiolite, NW Pacific Rim: From mid-ocean ridge spreading to tectonic accretion on land
- Climatic Controls on Alpine Rockwall Erosion: Current Rates Versus Long-Term Rates
- Numerical Simulation of the Arctic Oscillation by a Simple Barotropic Model with Baroclinic Eddies
- Sandstone Composition and Detrital Heavy Minerals from Sylhet Area, Bangladesh: Constraints on the Uplift History of the Himalayas
- Water-rock interaction observed in the Hatagawa fault zone, NE Japan: Impliccations for fluid characterization and fault activity in the brittle-plastic transition zone
- A numerical expariment of a topographic effect to Arctic oscillation by using barotropic global circulation model
- Deep-sea tsunami deposits in the Miocene Nishizaki Formation of Boso Peninsula, Central Japan
- En echelon knolls in the Nosappu Fracture Zone, NW Pacific: A possible leaky transform fault zone
- Fault Development In The Imbricate Thrust Pile Under Variable Basal Friction And Slope Geometry From The Sand Box Analog Modeling
- Fingerprinting the sources of fluvial sediment using fallout and in-situ radionuclides in forested watershed in Japan
- Overlandflow generation and surface erosion in Mongolia
- Structure and Tectonics of the Moho and Surrounding Part of the Oman Ophiolite, West Sohar
- The Implication of Structural Discontinuities in Rock Slope Stability Analysis: Example of Katsuura-Ubara, SE-Japan.
- Threshold conditions for channel initiation based on hydro-geomorphic observation in the eastern Ashio Mountains, Japan
- Water vapor transport to the Tibetan Plateau revealed with stable isotopes of precipitation: a new hypothesis for unusual isotope signals
- Water-weakened lower crust and its role in the concentrated deformation in the Japanese islands
- Accretionary Complex Origin of the Mafic-ultramafic Bodies of the Sanbagawa Belt, Central Shikoku, Japan
- Ocean Floor Metamorphism Recorded in the Taitao Ophiolite
- Re-Os Isotopic Systematics of the Taitao Ophiolite, Southern Chile
- Composition of Clay Minerals from Mudstones in the Nankai Accretionary Prism, Tenryu and Shiono-misaki Canyons
- Complex Seismic Source Inversion Method with the Data Covariance Matrix: Application to the 2010 Haiti Earthquake
- Fate of mass-transport deposits in convergent margins: Super- or sub-critical state in accretionary- or non-accretionary slope toes
- Change of sediment sources and hysteresis in suspended sediments due to surface decontamination in the Niida river catchment area affected by the Fukushima Daiichi nuclear power plant accident