Shintaro Abe
Biographic Data
| ID | 5584155 |
|---|---|
| NAME | Shintaro Abe |
| GIVEN NAMES | Shintaro |
| FAMILY NAME | Abe |
| SIGNATURE | ABE S |
| AFFILIATIONS | Association for the Development of Earthquake Prediction |
| VERIFIED | No |
| TOTAL WORKS | 3 |
| TOTAL CITATIONS | 0 |
| AUTHOR COUNT | 3 |
| EDITOR COUNT | 0 |
| FIRST PUBLICATION YEAR | 2023 |
| 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 …
Refraction Seismic Survey in Suruga Bay Using OBSs and Air-gun Sources
Suruga Bay is a tectonic bay that is traversed in the north-south direction by the Suruga Trough, which is considered to be a subduction boundary between the northern margin of the Philippine Sea Plate and the Eurasian Plate. In order to clarify the shape of the subducting plate boundary, seismic refraction surveys were conducted using 14 sets of pop-up type ocean bottom seismographs (OBSs) and air-guns as controlling seismic sources at a total o…
No prominent works on this page.
Refraction Seismic Survey in Suruga Bay Using OBSs and Air-gun Sources
Suruga Bay is a tectonic bay that is traversed in the north-south direction by the Suruga Trough, which is considered to be a subduction boundary between the northern margin of the Philippine Sea Plate and the Eurasian Plate. In order to clarify the shape of the subducting plate boundary, seismic refraction surveys were conducted using 14 sets of pop-up type ocean bottom seismographs (OBSs) and air-guns as controlling seismic sources at a total o…
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) · Geology (3 works) · Geology (3 works) · Seismology (3 works) · Tectonics (3 works) · Fault (geology) (2 works) · Geological and Geochemical Analysis (2 works) · High-pressure geophysics and materials (2 works) · Paleontology (2 works) · Paleontology (2 works)