Kenji KUSUNOKI
Biographic Data
| ID | 9510927 |
|---|---|
| NAME | Kenji KUSUNOKI |
| GIVEN NAMES | Kenji |
| FAMILY NAME | KUSUNOKI |
| SIGNATURE | KUSUNOKI K |
| AFFILIATIONS | Geological Institute, Faculty of Education, and Division of Technical Service, Shizuoka Branch, Shizuoka University |
| VERIFIED | No |
| TOTAL WORKS | 1 |
| TOTAL CITATIONS | 0 |
| WORKS AS AUTHOR | 1 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 2021 |
| LATEST PUBLICATION YEAR | 2021 |
| H-INDEX | 0 |
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…
Andesite (1 work) · Early Pleistocene (1 work) · earthquake and tectonic studies (1 work) · Geochemistry (1 work) · Geochronology (1 work) · Geological and Geochemical Analysis (1 work) · Geology (1 work) · Geology (1 work) · Geology and Paleoclimatology Research (1 work) · Geomorphology (1 work)