Go Sato
Biographic Data
| ID | 5975322 |
|---|---|
| NAME | Go Sato |
| GIVEN NAMES | Go |
| FAMILY NAME | Sato |
| SIGNATURE | SATO G |
| AFFILIATIONS | Tokyo City University |
| ORCID | 0000-0003-3426-8593 |
| VERIFIED | Yes |
| TOTAL WORKS | 3 |
| TOTAL CITATIONS | 0 |
| AUTHOR COUNT | 3 |
| EDITOR COUNT | 0 |
| FIRST PUBLICATION YEAR | 2022 |
| LATEST PUBLICATION YEAR | 2024 |
| H-INDEX | 0 |
Crustal Structure of the Northwestern Border of the Izu Collision Zone from the Fujikawa-kako Fault Zone to the Itoigawa–Shizuoka Tectonic Line, Central Japan
The Fujikawa-kako fault zone (FKFZ) is one of the most active fault zones constituting the northwest border of the Izu collision zone between the Honshu and Izu arcs. Although FKFZ has the highest vertical slip-rate in Japan, its structures in the seismogenic zone have not been sufficiently elucidated. In order to clarify the detailed structures, we carry out two stages of integrated seismic exploration. The first stage named FIST2012 is for reve…
Three-dimensional Structure of the Omiya and the Iriyamase Faults and Its Formation Process, the Eastern Margin of the Fujikawa-kako Fault Zone, the Northwestern Border of the Izu Collision Zone, Cent…
The Fujikawa-kako fault zone (FKFZ) is one of the most active fault zones constituting the northwest border of the Izu collision zone between the Honshu and Izu arcs. Its vertical slip rate is estimated to reach 6 to 7 m/ky along the eastern margin of FKFZ. In order to elucidate the causes of such high fault activities, the structure of this fault zone from the seismogenic zone to the surface is revealed. An integrated seismic exploration, which …
Simple Method for Shallow Landslide Prediction Based on Wide-Area Terrain Analysis Incorporated with Surface and Subsurface Flows
During intense rainfall, shallow landslides often occur on natural slopes due to the rising groundwater level. This study proposed a simple model for rainfall-induced shallow landslide prediction in broad areas based on an infinite homogeneous slope assumption and a simplified hydrological process. For this purpose, a numerical model, TAG_FLOW, was developed in Fortran 90. Its structure was divided into four modules: (1) a surface infiltration mo…
No prominent works on this page.
Simple Method for Shallow Landslide Prediction Based on Wide-Area Terrain Analysis Incorporated with Surface and Subsurface Flows
During intense rainfall, shallow landslides often occur on natural slopes due to the rising groundwater level. This study proposed a simple model for rainfall-induced shallow landslide prediction in broad areas based on an infinite homogeneous slope assumption and a simplified hydrological process. For this purpose, a numerical model, TAG_FLOW, was developed in Fortran 90. Its structure was divided into four modules: (1) a surface infiltration mo…
Crustal Structure of the Northwestern Border of the Izu Collision Zone from the Fujikawa-kako Fault Zone to the Itoigawa–Shizuoka Tectonic Line, Central Japan
The Fujikawa-kako fault zone (FKFZ) is one of the most active fault zones constituting the northwest border of the Izu collision zone between the Honshu and Izu arcs. Although FKFZ has the highest vertical slip-rate in Japan, its structures in the seismogenic zone have not been sufficiently elucidated. In order to clarify the detailed structures, we carry out two stages of integrated seismic exploration. The first stage named FIST2012 is for reve…
Three-dimensional Structure of the Omiya and the Iriyamase Faults and Its Formation Process, the Eastern Margin of the Fujikawa-kako Fault Zone, the Northwestern Border of the Izu Collision Zone, Cent…
The Fujikawa-kako fault zone (FKFZ) is one of the most active fault zones constituting the northwest border of the Izu collision zone between the Honshu and Izu arcs. Its vertical slip rate is estimated to reach 6 to 7 m/ky along the eastern margin of FKFZ. In order to elucidate the causes of such high fault activities, the structure of this fault zone from the seismogenic zone to the surface is revealed. An integrated seismic exploration, which …
Geology (3 works) · earthquake and tectonic studies (2 works) · Fault (geology) (2 works) · Geological and Geochemical Analysis (2 works) · Geology (2 works) · High-pressure geophysics and materials (2 works) · Paleontology (2 works) · Paleontology (2 works) · Seismology (2 works) · Stage (stratigraphy) (2 works)