GeoFEM : Multi-Purpose Parallel FEM for Solid Earth : (1) Project Overview
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概要
- 論文の詳細を見る
- 日本計算工学会の論文
- 1999-05-26
著者
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OKUDA Hiroshi
International Innovation Center, Kyoto University
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Okuda Hiroshi
The University Of Tokyo
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Yagawa Genki
Dept. Of Quantum Engineering And Systems Science University Of Tokyo
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NAKAMURA Hisashi
Research Organization for Information Science and Technology
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YAGAWA Genki
University of Tokyo
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OKUDA Hiroshi
Yokohama National University
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FUJISHIRO Issei
Ochanomizu University
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Okuda H
International Innovation Center Kyoto University
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Nakamura Hisashi
Research Center For Advanced Science And Technology University Of Tokyo
関連論文
- Degradation Mechanism of Amorphous Silicon Carbide Fiber due to Air-Exposure at High Temperatures
- Parallel Performance of GeoFEM and Its Applications to Solid Earth Problems
- Parallel Iterative Solvers for Unstructured Grids on SMP Cluster Architectures
- GeoFEM : Multi-Purpose Parallel FEM for Solid Earth : (1) Project Overview
- Analysis of Buckling and Interfacial Debonding of Galvannealed Coating Layer on Steel Substrates under Applied Tensile Strain
- The Effects of Solute and Vacancy Depletion on the Formation of Precipitation-Free Zone in a Model Binary Alloy Examined by a Monte Carlo Simulation
- An Efficient Finite Element Flow Analyses Applying the Biconjugate-Gradient Method and Hybrid/Multi-Level Meshes
- Large Scale FE Structural Vibration Analysis on Massive Parallel Computer
- A data interpretation for multi-objective multi-solution problems using clustering algorithm
- ICONE11-36537 AN EFFICIENT IMPLEMENTATION OF PARALLEL MOLECULAR DYNAMICS METHOD ON SMP CLUSTER ARCHITECTURE
- Crack Spacing Distribution in Coating Layer of Galvannealed Steel under Applied Tensile Strain
- A111 Factors contributing to precipitation changes simulated by IPCC-AR4 models under the A1B scenario
- First-Principles Calculations on Boron-Nitride Nanotubes(Condensed Matter : Electronic Structure, Electrical, Magnetic and Optical Properties)
- D109 Analysis of evaporation changes simulated by IPCC-AR4 models under the A1B scenario