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Nagaoka College of Technology | 論文
- Stratigraphic Analysis of Firn and Ice at Mizuho Station
- A Crack Kinked at the Interface of Bonded Anisotropic Elastic Media under Longitudinal Shear Stresses
- Formation of the High-T_c Phase of Bi_Pb_xSr_Ca_Cu_O_y (0 ≦ x ≦ 0.05)
- Influence of Intermediate Pressing on Superconducting Characteristics in Bi-Pb-Sr-Ca-Cu-O System
- Critical Current Density of Bi-Pb-Sr-Ca-Cu-O Superconducting Ceramics : Electrical Properties of Condensed Matter
- POLEX-SOUTH DATA, PART 6 AEROLOGICAL SOUNDING OF LOWER ATMOSPHERIC LAYER OVER MIZUHO PLATEAU, EAST ANTARCTICA
- POLEX-South data, Part 6 Aerological sounding of lower atmospheric layer over Mizuho Plateau, East Antarctica(Meteorology 17)
- Optical and Electrical Characterization of CuGaS_2 Grown by Vapor Phase Epitaxy
- Thickness change and flow of Tyndall Glacier, Patagonia
- Observation of GdBa_2Cu_3O_ Ceramic Microstructure : Electrical Properties of Condensed Matter
- Annual changes of snow accumulation in the coastal area near Syowa Station from analysis of firn cores (abstract)
- Meteorological features at Moreno and Tyndall glaciers, Patagonia, in the summer 1993/94
- Decay Characteristics of Photoluminescence Lines in CuGaS_2 Crystals
- Liquid Quenched Superconductor Ba-Y-Cu-O with T_=88 K and AC Josephson Effect at 77 K
- Study on Photoacoustic Signals from Powdered Samples
- On the scatter of snow accumulation measured at a given place on the Mizuho Plateau
- Transient Characteristics of Mobile Communication Traffic in a Band-Shaped Service Area (Special Section on JTC-CSCC '92)
- An Analysis of the Effect of a Stiffener Bonded to the Edge Surface of an Anisotropic Semi-Infinite Plate Containing an Internal Crack : Series A : Solid-Mechanics, Strength of Materials
- An Analysis of the Effect of a Stiffener Bonded to the Edge Surface of an Anisotropic Semi-Infinite Plate Containing an Internal Crack : Series A : Solid-Mechanics, Strength of Materials
- Interaction a between a Thin Elastic Stiffener and a Crack in an Anisotropic Half Space under Longitudinal Shear