The University of Tokyo
Earthquake research institute
In this study we have presented two-scale Generalized Finite Element (GFEM) for fracture analysis. GFEM is based on the enrichment of the classical FEM approximation. These enrichment functions incorporate the discontinuity response in... more
In this work, a sensitivity analysis of linear elastic cracked structures using two-scale Generalized Finite Element Method (GFEM) is presented. The method is based on computation of material derivatives, mutual potential energies, and... more
We present a high fidelity numerical simulation technique to analyze the collapse behavior of a composite beam under cyclic loading. The analysis is performed by utilizing the in-house software package called E-Simulator [1], which is... more
This paper presents the modelling and elasto-plastic analysis of E-Defense Shake Table test on soil-underground structure. Modified Cam-Clay model incorporating re-liquefaction phenomena by employing the concept of stress-anisotropy and... more
Soil-structure interaction plays a vital role in evaluation of seismic performance of structure. In this study, we present the systematic study of numerical and experimental results of large-scale experiment conducted at E-Defense.... more
The magma generation at Unzen volcano may be considered as the product of crustal material mixed with mantle magma Ž. accompanied by fractional crystallization AFC. The magma in the Unzen volcano is estimated to consist of about 50-80% Ž.... more
A buried, old volcanic body (pre-Komitake Volcano) was discovered during drilling into the northeastern flank of Mount Fuji. The pre-Komitake Volcano is characterized by hornblende-bearing andesite and dacite, in contrast to the... more
Anatahan Volcano, Northern Mariana Islands, began erupting in MayJune 2003. A series of subplinian explosive eruptions of andesite magma began at the Eastern Crater in the eastern part of the summit caldera on the evening of 10 May.... more
Large-scale collapse of a dacite dome in the late afternoon of 15 September 1991 generated a series of pyroclastic-flow events at Unzen Volcano. Pyroclastic flows with a volume of 1× 106 m3 (as DRE) descended the northeastern slope of the... more