Tatsuya Ishiyama
Biographic Data
| ID | 8878571 |
|---|---|
| NAME | Tatsuya Ishiyama |
| GIVEN NAMES | Tatsuya |
| FAMILY NAME | Ishiyama |
| SIGNATURE | ISHIYAMA T |
| AFFILIATIONS | Earthquake Research Institute, University of Tokyo |
| ORCID | 0000-0002-9376-8574 |
| VERIFIED | Yes |
| TOTAL WORKS | 3 |
| TOTAL CITATIONS | 0 |
| AUTHOR COUNT | 3 |
| EDITOR COUNT | 0 |
| FIRST PUBLICATION YEAR | 2024 |
| LATEST PUBLICATION YEAR | 2026 |
| H-INDEX | 0 |
Holocene sediments reveal accumulation rates across an onshore subduction thrust in northeastern Nankai Trough, Japan
The Fuji River flows approximately 128 km from north to south near the center of the Japanese archipelago, with its mouth located near the collision boundary between the Eurasian Plate and the Philippine Sea Plate. To investigate the Holocene activity of an onshore subduction thrust at the northern end of the Nankai Trough, we measured radiocarbon ages of terrestrial plants and marine shells in sediments collected from across the Fuji River. Ten …
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 …
No prominent works on this page.
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 …
Holocene sediments reveal accumulation rates across an onshore subduction thrust in northeastern Nankai Trough, Japan
The Fuji River flows approximately 128 km from north to south near the center of the Japanese archipelago, with its mouth located near the collision boundary between the Eurasian Plate and the Philippine Sea Plate. To investigate the Holocene activity of an onshore subduction thrust at the northern end of the Nankai Trough, we measured radiocarbon ages of terrestrial plants and marine shells in sediments collected from across the Fuji River. Ten …
earthquake and tectonic studies (3 works) · Fault (geology) (2 works) · Geological and Geochemical Analysis (2 works) · Geology (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)