
Yoshiya UsuiThe University of Tokyo | Todai · Earthquake Research Institute
Yoshiya Usui
Ph.D.
My research target is electrical resistivity structure modeling around fault zones and volcanoes.
About
19
Publications
3,314
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217
Citations
Citations since 2017
Introduction
I have developed a 3-D magnetotelluric inversion code (https://sites.google.com/view/yoshiyausui/femtic).
My research target is electrical resistivity structure modeling around fault zones and volcanoes.
Additional affiliations
April 2020 - present
November 2018 - March 2020
April 2010 - March 2020
ITOCHU Techno-Solutions Corporation
Position
- Engineer
Education
April 2014 - March 2017
April 2008 - March 2010
the University of Tokyo
Field of study
- Geo-Electromagnetics
Publications
Publications (19)
The southern part of Tohoku, Northeast Japan, is an area with significant in-land activities owing to the ongoing subduction mechanism. Among these are active volcanoes distributed on the volcanic front and back-arc, active faults throughout the area, and a recently observed swarm of shallow earthquakes on the fore-arc side. As fluids play an essen...
I tested the forward-calculation part by using the model of the seafloor with a 2-D sinusoidal undulation. Schwalenberg & Edwards (2004) and Usui et al. (2018) showed an analytical formulation for this model. Originally, Schwalenberg & Edwards proposed, and later, Usui et al. modified the formulation. I calculated the apparent resistivity, the phas...
The combined inversion using distortion-free response functions is an effective approach to robustly estimate the 3-D electrical resistivity structure against the distortions caused by near-surface resistivity anomalies. However, previous combined inversion analyses have presented a significant dependency of the inversion results on initial and pri...
Topographic distortion is a major problem in magnetotelluric modeling and interpretation. Especially, observed data of ocean magnetotelluric surveys can be affected by large-scale bathymetry and land-ocean distribution as well as smaller-scale seafloor undulations around observation sites. Some modeling approaches have been proposed to overcome the...
The Atotsugawa fault is one of the most active faults in Japan and the strain accumulation at the fault is considered to be caused by an aseismic shear zone in the fluid-rich lower crust. To identify the shear zone and investigate the origin of the aqueous fluid in the lower crust, we deployed a Network-MT survey in addition to a conventional wideb...
We aimed to perform three-dimensional imaging of the underlying geothermal system to a depth of 2 km using magnetotellurics (MT) at around the Yugama crater, the Kusatsu-Shirane Volcano, Japan, which is known to have frequent phreatic eruptions. We deployed 91 MT sites focusing around the peak area of 2 km × 2 km with typical spacings of 200 m. The...
In FBR plants the head plate constitutes a part of the boundary of the containment vessel (CV), therefore, it is a very important issue if the function as the boundary is maintained or not in the case of severe accident (SA). Buckling and post-buckling behaviors due to pressure loading must be affected by the thickness distribution of the head plat...
On 29 June 2015, a small phreatic eruption occurred at Hakone volcano, Central Japan, forming several vents in the Owakudani geothermal area on the northern slope of the central cones. Intense earthquake swarm activity and geodetic signals corresponding to the 2015 eruption were also observed within the Hakone caldera. To complement these observati...
The finite element method using an unstructured tetrahedral mesh is one of the most effective methods for the 3-D modelling of marine magnetotelluric data that are strongly affected by bathymetry, because it enables us to incorporate both small-scale and regional-scale bathymetry into a computational mesh with a practical number of elements. The au...
Asama Volcano is an andesitic composite volcano and one of the most active volcanoes in Japan. In order to reveal electrical resistivity structure beneath the volcano accurately, we performed a 3-D inversion of dense magnetotelluric survey data. In order to prevent misinterpretation of the subsurface resistivity due to the steep topography around A...
The finite element method using unstructured tetrahedral elements is one of the most effective methods to correct topographic distortions in the marine magnetotelluric data since it can precisely incorporate the bathymetry into computational grids without using too many elements. However, in relation to marine magnetotelluric problems, the use of h...
A 3-D magnetotelluric (MT) inversion code using unstructured tetrahedral elements has been developed in order to correct the topographic effect by directly incorporating it into computational grids. The electromagnetic field and response functions get distorted at the observation sites of MT surveys because of the undulating surface topography, and...
For the purpose of confirming failure modes and safety margin, some studies on the ultimate strength of thin-walled piping components for Sodium-cooled Fast Reactors (SFRs) under extreme loading conditions such as large earthquakes have been reported these several years. Nonlinear finite element analysis has been applied in these studies to simulat...
A resistivity section based on magnetotelluric data was obtained for the Shonai Plain fault in northeastern Honshu, Japan. Faults in this area were created as normal faults during the opening of the Japan Sea in the Miocene but are now reactivated as high-angle reverse faults under compressional tectonics. Geological interpretations of the resistiv...