Ken‐ichi Kano
Biographic Data
| ID | 10199678 |
|---|---|
| NAME | Ken‐ichi Kano |
| GIVEN NAMES | Ken‐ichi |
| FAMILY NAME | Kano |
| SIGNATURE | KANO K I |
| AFFILIATIONS | Shizuoka University |
| VERIFIED | No |
| TOTAL WORKS | 3 |
| TOTAL CITATIONS | 0 |
| AUTHOR COUNT | 3 |
| EDITOR COUNT | 0 |
| FIRST PUBLICATION YEAR | 2021 |
| 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 …
K–Ar Geochronology of the Andesite Lavas of the Lower Pleistocene Enrei Formation on the Southwestern Slope of the Suwa Basin, Central Japan
The Suwa Basin is believed to be a typical pull-apart basin formed by the 12 km left-lateral motion on the Itoigawa–Shizuoka Tectonic Line active fault system. The starting age of the basin subsidence is considered to be after the violent volcanisms that formed the Lower Pleistocene Enrei Formation (Fm) distributed in and around the basin. However, the history of the basin development is still controversial mainly because of the insufficient geoc…
No prominent works on this page.
K–Ar Geochronology of the Andesite Lavas of the Lower Pleistocene Enrei Formation on the Southwestern Slope of the Suwa Basin, Central Japan
The Suwa Basin is believed to be a typical pull-apart basin formed by the 12 km left-lateral motion on the Itoigawa–Shizuoka Tectonic Line active fault system. The starting age of the basin subsidence is considered to be after the violent volcanisms that formed the Lower Pleistocene Enrei Formation (Fm) distributed in and around the basin. However, the history of the basin development is still controversial mainly because of the insufficient geoc…
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 …
earthquake and tectonic studies (3 works) · Geological and Geochemical Analysis (3 works) · Geology (3 works) · Geology (3 works) · Paleontology (3 works) · Paleontology (3 works) · Fault (geology) (2 works) · High-pressure geophysics and materials (2 works) · Seismology (2 works) · Stage (stratigraphy) (2 works)